OD, pH and ammonium accumulation by
\r\n\tIn the maintenance and conservation of our planet's biodiversity, knowledge of current biogeographical patterns, speciation or invasion processes, flora, fauna, natural history, and ecology have outstanding importance. Many areas of biodiversity are still completely undiscovered nowadays. The ecological impacts of global climate change, urbanization, overpopulation, environmental pollution, deforestation, land cover and land-use changes also have a significant impact on biodiversity, flora, and fauna, through biogeographical patterns.
\r\n\tThe management tools, methods and processes (as applied ecological aspects) of Protected Areas and National Parks are a very important part of conservation policy. I am sure that this book will be very useful for everybody who would like to get some insight into the recent problems of biodiversity research, ecology and conservation biology also from practical or theoretical viewpoints.
Nitrogen is an essential element for many biological processes, including those occurring in plants (Ogura et al., 2006). Despite the abundance of atmospheric nitrogen, production of nitrogen fertilisers by the Harber–Bosch process is increasing annually due to the deficiency of ammonia produced by biological nitrogen fixation—the enzyme-catalyzed reduction of nitrogen gas (N2). Concern over ‘greenhouse’ gasses emitted by the Harber–Bosch process has resulted in a research focus on nitrogen-fixing bacteria, and in particular, their genetic modification to excrete excess ammonia for agricultural purposes (Terzaghi, 1980;Saikia& Jain, 2007).
\n\t\t\tThe nitrogen cycle.
There are three main biological processes in the natural cycle of nitrogen (Fig. 1): fixation, nitrification and denitrification, which involve nitrogen-fixing, nitrifying and denitrifying bacteria, respectively.
\n\t\t\tBlue arrows indicate nitrogen fixation, including biological and industrial processes. Green arrows indicate microbial nitrification processes involving nitrifying bacteria, and pink arrows indicate microbial denitrification processes involving denitrifying bacteria. Black arrows indicate the flow of each compound in soils. The NH3 produced by nitrogen fixation may be assimilated into amino acids and thence to protein and other N compounds, or it may be converted by nitrifying bacteria to NO2\n\t\t\t\t- and NO3\n\t\t\t\t-. In turn, NO3\n\t\t\t\t- may enter metabolism through reduction to NH4\n\t\t\t\t+ and subsequent assimilation to amino acids by bacteria, fungi and plants or can serve as an electron acceptor in denitrifying bacteria when oxygen is limiting. Losses from the nitrogen pool occur physically, when nitrogen (especially nitrate) is leached into inaccessible domains in the soils, and chemically, when denitrification releases N2.
\n\t\tDecomposers use several enzymes to break down proteins in dead organisms and their waste, releasing nitrogen in much the same way as they release carbon. Proteinases break large proteins into smaller molecules. Peptidases break peptide bonds to release amino acids. Deaminases remove amino groups from amino acids and release ammonia.
\n\t\t\tAccording to Kneip et al. (2007), during biological nitrogen fixation (BNF), molecular nitrogen is reduced (Formula 1) in multiple electron-transfer reactions, resulting in the synthesis of ammonia and release of hydrogen. Ammonium is then used for the subsequent synthesis of biomolecules. This reduction of molecular nitrogen to ammonium is catalysed in all nitrogen-fixing organisms via the nitrogenase enzyme complex in an ATP-dependent, highly energy-consuming reaction (Fig. 2). The nitrogenase complex is composed of two main functional subunits, dinitrogenase reductase (azoferredoxin) and dinitrogenase (molybdoferredoxin). The structural components of these subunits are the Nif (nitrogen fixation) proteins: NifH (γ2 homodimeric azoferredoxin) and NifD/K (α2β2 heterotetrameric molybdoferredoxin). Three basic types of nitrogenases are known based on the composition of their metal centres: iron and molybdenum (Fe/Mo), iron and vanadium (Fe/V) or iron only (Fe). The most common form is the Fe/Mo-type found incyanobacteria and rhizobia.Electrons are transferred from reduced ferredoxin (or flavodoxin) via azoferredoxin to molybdoferredoxin. Each mole of fixed nitrogen requires 16 moles ATP to be hydrolysed by the NifH protein. The NH3 produced is utilised in the synthesis of glutamine or glutamate for N-metabolism. NifJ: pyruvate flavodoxin/ferrodoxin oxidoreductase, NifF: flavodoxin/ferredoxin). An important feature of the nitrogenase enzyme complex is its extreme sensitivity to even minor concentrations of oxygen. In aerobic environments and in photoautotrophic cyanobacteria, in which oxygen is produced in the light reaction of photosynthesis, nitrogenase activity must be protected. This protection is mediated by different mechanisms in nitrogen-fixing bacteria, depending on their cellular and physiologic constitutions. Aerobic bacteria (like
Reactions and molecular mechanisms of biological nitrogen fixation.
General reaction of molecular nitrogen fixation. Schematic of the structure and operation of the nitrogenase enzyme complex and subsequent metabolism of nitrogen.
\n\t\t\t\n\t\t\t\t
Ultraviolet mutagenesis, the most easily controllable method of mutation, was thus often the first choice. Ultraviolet irradiation was used to modify
The same results arose from mutation of
With regard to the carbon sources used to culture these two species, most of the studies described above used Burk’s medium, which contains 2% sucrose, or modified Burk’s medium (0.5% or 2% glucose) as carbon sources. The latest researches on
To screen for nitrogen-fixing bacteria, 1 g of soil was suspended in 10 mL of sterilized dH2O in a 15-mL Eppendorff tube that was left to stand until the soil solution settled. A 1-mL aliquot of supernatant was then added to 200 mL of fresh NFMM or NFMM liquid medium and incubated for 1 week on a rotary shaker at 120 rpm and 30 C. Subculture was carried out twice by adding 2 mL of liquid culture to 200 mL of new C–NFMM medium and incubated as before. Single-colony isolation was performed on NFMM plates. Nitrogen-fixing activity was tested by growing the strains on glucose–NFMM plates substituted with BTB.From the 20 soil samples collected, we obtained four strains that showed a colour change in BTB-containing medium, suggesting excretion of ammonia. These strains were named C4, E4, G6 and G7.
\n\t\t\tDNA extraction was performed using a Miniprep DNA Purification Kit (TaKaRa). Bacterial 16S rDNA was amplified over 35 PCR cycles. Each cycle consisted of denaturation for 1 min at 94 C, annealing for 30 s at 60 C and extension for 4 min at 72 C. DNA purification was performed using the Agarose Gel DNA Extraction Kit (Roche Diagnostics GmbH). Ligation was conducted using the DNA Ligation Kit (TaKaRa) and the pT7 Blue T-vector (Novagen) as the plasmid. Transformation used
The nucleotide sequences of C4 and G7 showed high similarity (99%) to
RFLP analysis of the
RFLP of the amplified
\n\t\t\t\t
When wild-type
Ammonia concentration was estimated using the Visocolor Alpha Ammonia Detection Kit (Macherey-Nagel). After centrifugation at 13,000 rpm for 10 min at room temperature (RT), supernatant (1 mL) was transferred into a test tube. Two drops of NH4-1 were added to the sample and mixed well, after which one-fifth of a spoonful of NH4-2 was added. After mixing, the sample was left at RT for 5 min. One drop of NH4-3 was then added, mixed well and left at RT for 5 min.
\n\t\t\tAmmonia concentration was also estimated using ion chromatography. After centrifugation at 13,000 rpm for 10 min at RT, the supernatant was passed through a 0.2-μm filter and the ammonium concentration determined using an 861 Advanced Compact Ion Chromatography (Metrohm). The cation eluent used was 4 mM H3PO4 with 5 mM 18-crown 6-ether. The separation column was an IC YK-421 (Shodex) and the guard column was an IC-YK-G (Shodex). Standard ammonium solution was prepared from (NH4)2SO4; the concentration was adjusted to 1000 parts per million (ppm) and diluted appropriately to obtain a standard curve. All experiments were performed in triplicate.
\n\t\t\n\t\t\t\t
The optimum carbon source concentration was used to determine the correlations among incubation time, ammonia accumulation and carbon uptake.
Glucose concentration | \n\t\t\t\t\t\t\n\t\t\t\t\t\t | 0.10% | \n\t\t\t\t\t\t0.25% | \n\t\t\t\t\t\t0.50% | \n\t\t\t\t\t\t0.70% | \n\t\t\t\t\t\t1.00% | \n\t\t\t\t\t\t2.00% | \n\t\t\t\t\t
A. beijerinckii | \n\t\t\t\t\t\tOD pH NH4\n\t\t\t\t\t\t\t+\n\t\t\t\t\t\t | \n\t\t\t\t\t\t0.145 7.0 (7.0)* 0.062 | \n\t\t\t\t\t\t0.486 7.0 (7.0)* 0.117 | \n\t\t\t\t\t\t1.109 6.8 (7.1)* 0.202 | \n\t\t\t\t\t\t1.406 6.6 (7.1)* 0.080 | \n\t\t\t\t\t\t1.698 6.4 (7.1)* 0.026 | \n\t\t\t\t\t\t1.522 6.3 (7.1)* 0.001 | \n\t\t\t\t\t
A. vinelandii | \n\t\t\t\t\t\tOD pH NH4\n\t\t\t\t\t\t\t+\n\t\t\t\t\t\t | \n\t\t\t\t\t\t0.189 7.1 (7.1)* 0.010 | \n\t\t\t\t\t\t0.478 6.8 (7.1)* 0.024 | \n\t\t\t\t\t\t0.950 6.1 (7.1)* 0.020 | \n\t\t\t\t\t\t1.391 4.9 (7.1)* 0 | \n\t\t\t\t\t\t1.710 4.7 (7.1)* 0 | \n\t\t\t\t\t\t1.948 4.7 (7.0)* 0 | \n\t\t\t\t\t
OD: optical density (600 nm). *Figures in parentheses show the value before incubation. | \n\t\t\t\t\t|||||||
Note: ammonium ion concentration is in mM. Presence of ammonium was primarily tested using Nesler’s reagent before the concentration was determined by ion chromatography. | \n\t\t\t\t\t
OD, pH and ammonium accumulation by
\n\t\t\t\t\t\t | \n\t\t\t\t\t\t | Glucose | \n\t\t\t\t\t\tFructose | \n\t\t\t\t\t\tGalactose | \n\t\t\t\t\t\tMannose | \n\t\t\t\t\t\tSucrose | \n\t\t\t\t\t\tCitrate | \n\t\t\t\t\t\tSuccinate | \n\t\t\t\t\t
A. beijerinckii | \n\t\t\t\t\t\tOD | \n\t\t\t\t\t\t0.518 | \n\t\t\t\t\t\t0.739 | \n\t\t\t\t\t\t0.564 | \n\t\t\t\t\t\t0.029 | \n\t\t\t\t\t\t0.656 | \n\t\t\t\t\t\t0.005 | \n\t\t\t\t\t\t0.212 | \n\t\t\t\t\t
pH | \n\t\t\t\t\t\t7.3 (7.0)* | \n\t\t\t\t\t\t7.2 (7.0)* | \n\t\t\t\t\t\t7.1 (7.1)* | \n\t\t\t\t\t\t7.1 (7.1)* | \n\t\t\t\t\t\t7.1(7.1)* | \n\t\t\t\t\t\t7.4 | \n\t\t\t\t\t\t8.6 (7.2)* | \n\t\t\t\t\t|
NH4+ | \n\t\t\t\t\t\t0.296 | \n\t\t\t\t\t\t0.315 | \n\t\t\t\t\t\t0.201 | \n\t\t\t\t\t\t0.041 | \n\t\t\t\t\t\t0.192 | \n\t\t\t\t\t\t(7.0)* | \n\t\t\t\t\t\tN. D. | \n\t\t\t\t\t|
\n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | N. D. | \n\t\t\t\t\t\t\n\t\t\t\t\t | |
A. vinelandii | \n\t\t\t\t\t\tOD | \n\t\t\t\t\t\t0.442 | \n\t\t\t\t\t\t0.704 | \n\t\t\t\t\t\t0.573 | \n\t\t\t\t\t\t0.122 | \n\t\t\t\t\t\t0.655 | \n\t\t\t\t\t\t0.361 | \n\t\t\t\t\t\t0.361 | \n\t\t\t\t\t
pH | \n\t\t\t\t\t\t7.0 (7.0)* | \n\t\t\t\t\t\t7.2 (6.9)* | \n\t\t\t\t\t\t7.1 (7.0)* | \n\t\t\t\t\t\t7.1 (7.1)* | \n\t\t\t\t\t\t7.2(7.0)* | \n\t\t\t\t\t\t8.4 | \n\t\t\t\t\t\t8.8 (7.2)* | \n\t\t\t\t\t|
NH4+ | \n\t\t\t\t\t\t0.026 | \n\t\t\t\t\t\t0.179 | \n\t\t\t\t\t\t0.025 | \n\t\t\t\t\t\t0.017 | \n\t\t\t\t\t\t0.63 | \n\t\t\t\t\t\t(7.0)* | \n\t\t\t\t\t\tN. D. | \n\t\t\t\t\t|
\n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | \n\t\t\t\t\t\t | N. D. | \n\t\t\t\t\t\t\n\t\t\t\t\t | |
N.D.: not determined, OD: optical density (600 nm). *Figures in parentheses show the value before incubation. | \n\t\t\t\t\t||||||||
Note: ammonium ion concentration is in mM. Presence of ammonium was primarily tested using Nesler’s reagent before the concentration was determined by ion chromatography. | \n\t\t\t\t\t
OD, pH and ammonium accumulation by
A: Growth (■), pH (▲), ammonium concentration of
As the
Time-course experiments suggested that ammonia accumulation began upon glucose depletion. In the 0.30% medium, no glucose remained after incubation for 3 days, resulting in ammonia accumulation. In media with higher glucose concentrations, residual glucose was present after 3 days. As a result, no ammonia accumulation occurred; longer incubation times may have resulted in production of detectable levels of ammonia (Fig. 5A).
\n\t\t\tA: Growth (■), pH (▲), ammonium concentration of
Residual sugar levels were determined using a glucose detection kit, according to the manufacturer’s protocol (Miwa et. al., 1972). For
These data suggest that ammonia accumulation by strain E4 is dependent on sugar concentration. Glucose is required for bacterial growth until the middle of the logarithmic phase, and fixation of nitrogen during this period likely supports bacterial growth. Ammonia starts to accumulate when no more glucose remains in the culture, as shown by glucose and ammonia determinations after 14 h incubation (Fig. 5B).
\n\t\t\tFor
Thus, in both strains, ammonia began to accumulate at the end of log phase or in early stationary phase; no carbon source could be detected in the medium at this time. Higher ammonia levels in the medium will likely be detected after moreover 30 hours, longer incubation times, suggesting that the mechanism of nitrogen fixation might be influenced by sugar levels in the medium.
\n\t\t\tE4 strain grew well at pH 7.0 and produced the highest concentration of ammonia (~0.4 mM). Although media at pH 8.0 resulted in the greatest growth, ammonia accumulation was lower than at pH 7.0, suggesting that accumulated ammonia at the higher pH value may have been used for bacterial growth (Fig. 5B).
\n\t\t\tAmmonia was detected in E4 cultures incubated at 30 C, but not at 20 C. Ammonia may accumulate at 20 C after longer incubation times, since some glucose remained after 3 days incubation.
\n\t\tFrom the above, the following conclusions could be drawn. Firstly, the ammonium accumulation is clearly dependent on the carbon source concentration. Higher ammonium accumulation occurred in media with lower concentrations of the carbon source. Glucose was required for growth of
The Japanese Islands are mainly composed of the Eurasian (EUR) and the North American (NA) plates, and a number of small islands are on the Philippine Sea (PHS) and the Pacific (PAC) plates (Figure 1). The PHS and PAC oceanic plates are subducting beneath the EUR and the NA plates. A number of earthquakes occurred both at the plate interfaces and within the plates.
\nName of plates and location.
After the Kobe earthquake in January 1995, the Japanese government enacted the Special Measure Law on Earthquake Disaster Prevention in July 1995. This was to promote a comprehensive national policy on earthquake disaster prevention. Based on this goal, the National Research Institute for Earth Science and Disaster Resilience (NIED) contracted the deployment of the nationwide high-sensitivity seismograph network (Hi-net) [1] since NIED had already accumulated the experience for the Tokyo metropolitan deep borehole array and operated the Kanto-Tokai seismic network since 1979. NIED operates the Hi-net with approximately 800 stations since 2000 [2] and the full range seismograph network (F-net) [3] with approximately 70 stations composed of broadband seismographs since 1994 [4]. The Japan Meteorological Agency (JMA), the national universities, and other institutes operate other seismic networks with a total of approximately 600 stations for the detection of microseismicity. NIED operates ocean-bottom seismic stations beneath the Sagami Bay, while the JMA operates offshore the Tokai and Boso regions. The Earthquake Research Institute, University of Tokyo, operates the network offshore Sanriku, and the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) operates offshore Kushiro and Muroto networks. JAMSTEC started the construction of the Dense Oceanfloor Network System for Earthquakes and Tsunamis (DONET) [5] off Kii and Muroto Peninsulas near the Nankai Trough in 2010, and they started operation networks offshore Kii (in 2014) and Muroto (in 2016) Peninsulas. NIED deployed the Seafloor Observation Network for Earthquakes and Tsunamis along the Japan Trench (S-net) [6] after the 2011 offshore Tohoku Earthquake (the Tohoku-oki event), which began operating in 2016 [7, 8]. DONET was transferred to NIED from April 2016. NIED started the operation of Monitoring of Waves on Land and Seafloor (MOWLAS) composed of Hi-net, F-net, S-net, DONET, strong-motion seismograph networks (K-NET and KiK-net) [9], and Volcano Observation Network (V-net) [10].
\nNIED S-net and DONET teams manually pick the arrival time data at the oceanic seismic stations after NIED Hi-net team has determined the hypocenters using the land stations. We confirm the difference of shallow hypocenters between the determination by only NIED Hi-net and that by NIED Hi-net and NIED S-net. Stars in Figure 2 show the hypocenters at depths shallower than 20 km beneath the PAC plate determined by NIED Hi-net from September 11, 2017, to the end of 2018. The shallow hypocenters near the main island tend to remain shallow; however, hypocenters more than 200 km off the coast shifted significantly deeper to 40–80 km depth when including the S-net arrival time data (Figure 2). Deep events determined by NIED Hi-net on the east side of a longitude of 144°E are also shifted shallower. This suggests that it is important to include the S-net data for reliable hypocenter locations of offshore events.
\nComparison of hypocenters determined by the NIED (a) Hi-net and (b) Hi-net and S-net. Stars denote hypocenters determined at depths shallower than 20 km by only Hi-net in (a) and redetermined by Hi-net and S-net in (b).
Three-dimensional (3D) seismic velocity structure beneath the whole Japanese Islands has been studied using the vast data of seismic stations within the Japanese Islands maintained by NIED, JMA, national universities, and the other national and local governmental institutes (e.g., [11, 12, 13, 14]). These studies used data obtained mainly at land-based seismic stations with a very few seismic stations on the sea floor such as Sagami Bay, off Kushiro, Sanriku, Boso, and Tokai regions. Reference [14] investigated the structure beneath the PAC plate at depths of 30–50 km using events that occurred under the Pacific Ocean (PO) with focal depths determined by NIED F-net. However, that study was not able to clarify the shallow structure beneath the PO at depths of 0–20 km because of the lack of seismic stations on the seafloor of the PO. The seismic ray takeoff angles proceed downward from the events to the seismic stations on land, and they do not pass through the shallow zone beneath the ocean since the distance from the hypocenter to the seismic stations is usually over 150 km. We investigated the 3D seismic velocity structure of and around Japanese Islands including the Sea of Japan and PO by the seismic tomographic method. We added the arrival time data detected in the S-net, the DONET, and the Hi-net datasets, operated by NIED, as well as other datasets, operated by multiple organizations, after 2016 in addition to the data used in [14]. Then we applied the seismic tomography to these datasets.
\nThe target region, 20–48°N and 120–148°E, covers the whole Japanese Islands from Hokkaido to Okinawa and the seismic stations both Hi-net on land and S-net and DONET beneath the ocean. In addition to the arrival time data used by [14], 1,782,425 P- and 1,528,733 S-wave arrival times from 32,952 earthquakes recorded at approximately 2000 stations including NIED S-net and DONET from April 2016 to June 2018 were selected. A total of 7,853,757 P-wave arrival data and 4,604,780 S-wave arrival data from 112,631 events are available after merging the new datasets (Figure 3).
\nDistribution of hypocenters and seismic stations used for seismic tomography.
We used the seismic tomographic method [15, 16] with spatial velocity correlation and station corrections to the original code by [11]. Grid nodes were placed with half of the spatial resolution. We performed smoothing in order to stabilize the solution for the inverse problem with the LSQR algorithm [17] since arbitrary damping matrix with combination of diagonal and smoothing matrices could be assumed.
\nWe placed 3D grid nodes to construct the velocity (slowness) structure with the grid spacing shown in Table 1 and adopted the 1D structure used in the routine determination of hypocenters at the Hi-net and S-net [18] as the initial velocity model (Figure 4). No velocity discontinuities such as Moho discontinuities or the plate boundary between the EUR and PAC or PHS plates were assumed in this study. This is because there were enough data to estimate the steep velocity gradient to represent plate boundaries so that velocity discontinues in the model were not necessary [13, 16, 19]. The total number of unknowns, 4,417,505, for P-wave slowness is the same as those for S-wave slowness. We solved the P- and S-wave slowness at each grid node from more than 10 associated rays.
\nDepth | \nGrid interval | \nResolution/checkerboard pattern | \n||
---|---|---|---|---|
Horizontal | \nVertical (km) | \nHorizontal | \nVertical (km) | \n|
0–10 | \n0.1° | \n2.5 | \n0.2° | \n5 | \n
10–40 | \n5 | \n10 | \n||
40–60 | \n10 | \n20 | \n||
60–180 | \n15 | \n30 | \n||
180–300 | \n20 | \n40 | \n||
300− | \n25 | \n50 | \n
Grid interval and resolution size.
Seismic velocity structures of the initial model and the average of the final 3D model.
First, we inverted the P- and S-wave seismic velocities using the initial hypocenter location. Second, both hypocenters and 3D seismic velocity structure were inverted simultaneously. We included the arrival times from the events beneath the ocean before 2015 in addition to the data used by [14]. Focal depths of offshore events were determined by NIED F-net or [20] since offshore events determined by only NIED Hi-net are not reliable. For these offshore events, only epicenters are inverted by the 3D seismic velocity structure, while hypocenter depths are fixed. We do not fix any condition for the events after 2016 detected by NIED S-net and DONET and the events within 50 km of the onshore seismic networks before 2015 during the inversion.
\nResiduals are improved to within 0.5 s for P-wave and 0.6 s for S-wave in the travel time inversion. In the final iteration, we used 6,356,481 P-wave arrival data and 3,534,482 S-wave arrival data to solve for the P-wave slowness at 1,135,165 grid nodes and the S-wave slowness at 1,103,525 grid nodes. The inversion reduces RMS of the P-wave travel time residual from 0.561 to 0.192 s and that of the S-wave data from 0.812 to 0.239 s after 11 iterations.
\nWe conducted a checkerboard resolution test to evaluate the reliability of our solution [21]. We assumed a ± 5% checkerboard pattern and calculated synthetic travel times with random noise of 0 mean and standard deviations of 0.13 and 0.24 s for P- and S-waves, respectively. The standard deviations for random noise were derived from the average of the estimated uncertainty of the manually picked arrival times. The weight of data is inversely proportional to each width of picking error. The damping factors for the P-wave inversion are twice those for the S-wave inversion, since the average standard deviation of P-wave picking errors is almost half of that of S-wave.
\nFigure 5 shows the results of checkerboard resolution test. We calculate the recovery rate and stability with surrounding grid nodes in order to confirm well-resolved area [15]. The resolutions of Vp and Vs at depths of 5–30 km beneath main four islands are good. At depths of 40–60 km, resolutions are not good along the Sea of Japan coast because there are few deep earthquakes that can be used for inversion.
\nMap views of checkerboard resolution test for Vp and Vs. green line surrounds the well-resolved area.
NIED S-net data increase the resolution at depths of 10–60 km from Honshu to the Japan Trench (Figure 5). Reference [14] used the offshore events such as aftershocks of the Tohoku-oki earthquake. The presence of a seismic station above the events is extremely important for the estimation of velocity structure as well as the determination of hypocenters. The resolutions at depths of 0 and 5 km are still not good in spite of the use of S-net data because the incident angle to the S-net stations are mainly steep and ray paths do not run horizontally because of the lack of shallow earthquakes. Resolutions near the triple junction of Japan Trench and Sagami Trough where three plates, PAC, PHS, and EUR, meet are good at depths of 20–30 km. This is an advantage of using NIED S-net.
\nBeneath the DONET area, the resolution at depths of 10–60 km is good for Vp, and those at depths of 5–40 km are good for Vs. The resolved zone extends to the Nankai Trough since there is sufficient seismicity in this area.
\nWe calculated the average 1D model from the final 3D velocity structure (Figure 4). We also showed the perturbation from these average velocities (Figure 6).
\nMap views of Vp and Vs perturbation and Vp/Vs. Colored area is the resolved area. Broken white lines at depths of 10 and 20 km denote the median tectonic line.
At a depth of 5 km, low-Vp and low-Vs regions are located along the PAC coast beneath southeastern Hokkaido, northeastern Honshu, most of Kanto, Sagami Bay, southern Kinki, and southern Shikoku regions. A low-Vs region extends beneath the entire Shikoku and southern Chugoku regions. A low-Vp/Vs region runs along the Ou backbone range in northeastern Japan and central Japan. Other regions have high Vp/Vs.
\nAt a depth of 10 km, low-Vp regions extend beneath the active volcanoes in the northeastern and central Honshu and Kyushu regions. Low-Vs regions are almost the same as those at a depth of 5 km. High-Vp/Vs regions are distributed at central Hokkaido and coastal area in northeastern Japan. Low-Vp/Vs covers the other regions.
\nAt a depth of 20 km, low-Vp regions lie beneath volcanoes in Hokkaido, central Honshu, and Kyushu. Low-Vs regions extend beneath the volcanoes and back-arc side of Honshu. Both low-Vp and low-Vs regions extend from central Kinki to Kyushu region across central Shikoku. This low-V zone remains the same as at a depth of 5 km. High-Vp/Vs regions cover the Ou backbone range and back-arc side of northeastern Honshu.
\nAt a depth of 30 km, low-Vp extends beneath the northeastern Honshu, central and southwestern Honshu, and northern Kyushu regions. Low-Vs regions extend beneath most of Honshu, Kyushu, and northern Shikoku regions. High-Vp/Vs regions cover almost all Japanese Islands except the central Hokkaido.
\nAt a depth of 40 km, low-Vp regions exist beneath the volcanoes in southeastern Hokkaido and northeastern and central Honshu regions. The low-Vp regions beneath the volcanoes in the northeastern Japan extend to back-arc side. Low-Vs regions are clarified beneath the volcanoes in southeastern Hokkaido and central Honshu regions. Low-Vs regions beneath the northeastern Honshu can be found east of the volcanic front as are low-Vp regions. Low-Vp/Vs regions cover the central mountains across Hokkaido and northeastern and central Honshu.
\nAt a depth of 60 km, low-Vp and low-Vs regions extend beneath the volcanoes in Honshu and central Honshu. High-Vp and Vs regions extend beneath the Kinki, Shikoku, and eastern Kyushu regions where the PHS plates subduct. High-Vp/Vs regions are distributed across western Hokkaido, central Honshu, and central Shikoku regions.
\nAt a depth of 90 km, low-Vp and low-Vs regions exist beneath the volcanoes beneath Hokkaido and Honshu. High-Vp and Vs regions extend to the east of northeastern Japan where the PAC plate subducts. High-Vp/Vs regions cover northern and southwestern Hokkaido, central Honshu, and central Kyushu regions.
\nAt a depth of 10 km, a low-Vp and low-Vs zone extends along the coast of the PO in the northeastern Honshu. A high-Vp and high-Vs zone exists between the longitudes of 142 and 143°. East of longitude of 143° (Figure 6A and B), low-Vp, and low-Vs zone shows again. Vp/Vs is generally low except in some small regions.
\nAt a depth of 20 km, a high-Vp and high-Vs zone extends along the coast of the PO in the northeastern Honshu, in contrast to the structure at a depth of 10 km. Low-V zones extend to the east of the high-Vp zone; however, some high-Vp zones exist among the low-Vp zones (Figure 6C). High-Vs zones are mixed with minor low-Vs zone off the east of northeastern Honshu, extending to a longitude of 143.5° (Figure 6D). This pattern can be seen with Vp at a depth of 10 km. Vp/Vs is also broadly low, and this pattern of Vp/Vs can be seen when the depth is 10 km except in some regions.
\nAt a depth of 30 km, low-Vp zone extends off the east of northeastern Honshu between longitudes of 142 and 143.5 and to the region off the southeast of Hokkaido. High-Vp zone can be seen along the Japan Trench. Two patches of low-Vs zones exist in the east of northeastern Honshu at latitude of 37–40° and longitude of 142–143° and at latitude of 35–36° and longitude of 141–142°. High-Vp/Vs region is bounded by the low-Vp/Vs region, a north–south “stripe” pattern.
\nAt a depth of 40 km, low-Vp and low-Vs zones extend between longitude of 142–143° and latitudes of 37–41°. These low-Vp and low-Vs zones extend to the west of the Hidaka Mountains. High-Vp and high-Vs zones can be seen on the east of the low-V zone and reach the east of the Japan Trench. Vp/Vs in this area is moderate except for some low-Vp/Vs regions with north–south trend.
\nAt a depth of 60 km, low-Vp and low-Vs zones extend just off the coast of the PAC in the northeastern Honshu. High-Vp and high-Vs zones extend broadly on the east of the narrow low-V zone. Vp/Vs in this area is high.
\nAt depths of 20 and 30 km, low-Vp zones extend around the hypocenters of the large events with magnitude 6.9 and 7.4 that occurred on September 5, 2004. Low-Vs zones partly exist within the low-Vp zone. We cannot resolve the continuous structure from Honshu at depths of 5–10 km since the number of events for seismic tomography beneath the DONET stations is small. This is because the DONET picked data are basically added after the Hi-net manual picking. The seismic tomography will be recalculated when the microearthquake data triggered at DONET stations become available.
\nThe station corrections for the final model are shown in Figure 7. Red stations denote positive O-C travel times. It means that the modeled velocity is too high due to thick sediment or low-V materials since the calculated travel time is too small. It also depends on the depth of borehole of Hi-net stations. The seismometers of the Hi-net stations are typically deployed at depths of around 100–200 m, and low-Vp sediment materials are estimated beneath the backbone range and back-arc side of Japan. Large station corrections are estimated along the Sea of Japan coast in northeastern Honshu since there are thick sediments, while borehole stations are relatively shallow. For Vs, there are many blue-colored stations meaning that the velocity model is too slow. Large station corrections are also estimated on the Sea of Japan side of northeastern Honshu.
\nStation corrections for (a) Vp and (b) Vs.
For S-net stations, blue stations can be seen near the coast and the Japan Trench. Red stations are shown between them for both Vp and Vs. It suggests that the seismic velocity model is too slow near the coast and the Japan Trench and too fast between them.
\nFor DONET stations, red stations are shown near the coast and blue stations reside off the coast. It means that the modeled seismic velocity is too high near the coast.
\nFigure 8 shows the histogram of the epicentral movement during the iterations. Epicenters determined by NIED F-net and [20] are shifted over 50 km after the inversion. Epicenters determined by NIED Hi-net or by NIED Hi-net, S-net, and DONET are mainly less than 10 km in spite of 11 iterations of inversion.
\nHistogram of the earthquake epicentral movements during the inversion. The initial epicenters are determined by (a) NIED Hi-net; (b) NIED Hi-net, S-net, and DONET; (c) NIED F-net; and (d) Ref. [
Ref. [14] also clarified the seismic velocity structure beneath the PO at depths of 30–50 km; however, that study could not resolve the shallow structure at depths of 0–20 km since the ray paths, such as head waves, from the oceanic event to the land seismic stations pass through the deep zone. The ray paths from the events to NIED S-net stations run through the shallow part of the PO. In this study, we can clarify the structure at depths of 10–60 km and even east of the Japan Trench at depths of 20–30 km (Figures 5 and 6). This is a major improvement enabled by including NIED S-net data
\nOne important feature is the probable Mesozoic rift structure trending NS from the coast of Tohoku to the west of Hidaka Collision Zone. The recent 2018 Hokkaido Eastern Iburi earthquake (M6.7) (Iburi earthquake) occurred at a depth of around 32 km, which is much deeper than the usual inland crustal earthquake. Unfortunately, the structure beneath the PO between the Honshu and Hokkaido islands at a depth of 20 km is not clear; however, a low-Vp zone at a depth of 30 km in north–south direction between 142 and 143° (Figure 9) is resolved. Low-Vp zones also exist west of the Hidaka Mountains and between the Honshu and Hokkaido at the northern extension of this low-V zone, although the high-Vp zone parallel to the Japan Trench along the coast of Honshu and Hokkaido invades the low-Vp zone. The high-Vp zone is consistent with the large positive Bouguer gravity anomaly [22] and large positive aeromagnetic anomaly zones [23]. It implies that high-V mantle mafic material is located in the shallow zone. The depth of the Moho is also shallow near the coast of northern Honshu [24]. The Iburi earthquake may be related to the reactivation of the rift related to the structure in the upper mantle to the lower crust, where it is marked by high-Vp.
\nMap views of (a) Moho depth, (b) aeromagnetism, (c) Bouguer gravity anomaly, Vp perturbation at depths of (d) 20 km and (e) 30 km beneath northern Japan.
We clarified the seismic velocity structure beneath the Sea of Japan at depths of 10–20 km from offshore Hokkaido to Wakasa Bay (Figure 6). The Vp beneath the Okushiri and Sado Islands is low at a depth of 10 km; however, Vp beneath the Sea of Japan is high at depths of 10–35 km. Vp along the coast of Sea of Japan in western Japan gives moderate value. The lithospheric velocity structure in this region is strongly affected by the Mid-Tertiary breakup and formation of the Sea of Japan. Through the reactivation of the younger compressed tectonic terrain, tsunamigenic source faults have been developed. The lithospheric structure provides essential information to infer the structure of faults.
\nRef. [25] imaged the bending-shaped low-Vp oceanic crust of PAC plate subducting from the Japan Trench at latitudes of 38–38.5° offshore Miyagi where the rupture of large interplate earthquakes propagated. In this study, low-Vp material is imaged at depths of 40–50 km bounded by the high-Vp materials with a number of earthquakes surrounded with red ellipse in Figure 10. It indicates the subducting oceanic crust of the PAC plate
\nVertical cross section beneath the Pacific Ocean off Miyagi in WNW-ESE direction. Black circle shows the relocated hypocenters used for seismic tomography in this study.
The isovelocity contour of Vp = 7.0 km/s lies around depths of 25–40 km. Active-source seismic experiments off Sanriku region imaged the same contour lying at depths of 20–35 km [25] on the west side of Japan Trench, at depths of 15–30 km at the Japan Trench [26], and at depths of 15–25 km in NS direction between Honshu and Japan Trench [27]. The seismic velocity model of this study is relatively slower than those models derived from seismic experiments. The difference may depend on the initial velocity model of the oceanic region being set as the same as the land area in this study. The Moho depth becomes shallower with the EUR crust toward the Japan Trench. The oceanic crust of the PAC plate has also thinner crust than the EUR island arc crust.
\nFigure 11 shows the Vp perturbation just above the upper boundary of the PAC plate within the overriding EUR plate. The plane with the upper side at surface has a dip angle of 15°. Reference [28] also showed the Vp perturbation [29] above the upper boundary of the subducting PAC slab and three low-V zone offshore Sanriku, Miyagi, and Ibaraki. In our results, we obtain velocity structure in fine scale; however, we do not estimate the shallow structure along the Japan Trench. We obtain the broad low-Vp and low-Vp/Vs zone within the overriding EUR plate between the Japan Trench and Honshu. A high-Vp and slightly high-Vp/Vs zone exists on the west side of the low-Vp and low-Vp/Vs zone. There are some small high-V zones within the low-V zone near the hypocenter of the Tohoku-oki event.
\nVp perturbation on the plane just above the upper boundary of the PAC plate within the overriding EUR plate. The plane has strike with S17degW from the point with a longitude of 144.5 and a latitude of 41.0 with dip angle of 12 deg. The depth of the upper edge of the plane is 10 km.
Figure 12 also shows the Vp perturbation and Vp/Vs on the coseismic plane of the Tohoku-oki event [30]. We do not obtain the shallow structure along the Japan Trench although the extremely large slip of the Tohoku-oki event is estimated near the Japan Trench. The western edge of the large slip zone is consistent with the high-Vp zone; however, the surrounding region has low-Vp and low-Vp/Vs. Low-Vp/Vs material is difficult to deform so that it can generate large elastic waves if it fails. Low-Vp/Vs on the coseismic slip region may be one of the reasons for the extreme size of the Tohoku-oki event.
\n(a) Vp perturbation and (b) Vp/Vs on the coseismic slip plane [
We conducted the seismic tomography for entire Japanese Islands including oceanic area. This is the first tomographic study to use the data from NIED S-net. The hypocenters of oceanic events are greatly improved using the S-net data. We also obtain the detailed seismic velocity structure beneath the PO at depths of 10–60 km. Low-Vp and low-Vs zones are revealed between 142 and 143° at a depth of 30 km and in western Hokkaido where the Eastern Iburi Earthquake in 2018 occurred. The lithospheric velocity structure on the coast of Sea of Japan on Honshu is strongly affected by the Mid-Tertiary breakup and formation of the Sea of Japan. Tsunamigenic source faults have been developed through the reactivation of the younger compression. Subducting low-V oceanic crust is imaged within the mantle of overriding EUR and subducting oceanic PAC plate. The coseismic slip plane of the Tohoku-oki event has low-Vp/Vs; however, the shallow structure along the Japan Trench will be improved in the future with increased data. Previous seismic reflection and refraction studies found the oceanic crust at the uppermost part of the PAC plate with Vp of approximately 6–7 km/s; however, the seismic tomography with NIED S-net clarified the 6–7 km/s Vp zone at depths of 25–40 km. The result may depend on the initial velocity model beneath the PO, which was the same initial model as the land area in this study. Applying the initial velocity model derived from the refraction or reflection seismology would improve the results beneath the ocean in the future.
\nWe used the seismic data provided by the National Research Institute for Earth Science and Disaster Resilience, the Japan Meteorological Agency, Hokkaido University, Hirosaki University, Tohoku University, the University of Tokyo, Nagoya University, Kyoto University, Kochi University, Kyushu University, Kagoshima University, the National Institute of Advanced Industrial Science and Technology, the Geographical Survey Institute, Tokyo Metropolis, Shizuoka Prefecture, Hot Springs Research Institute of Kanagawa Prefecture, Yokohama City, and Japan Agency for Marine-Earth Science and Technology. This study was supported by the project on the Operation of Seismograph Networks for NIED. We thank academic editor Masaki Kanao for checking and commenting on our manuscript. We also thank David Shelly and Tomoko E. Yano for their helpful comments and improvement of our manuscript. Some of the figures were drawn using Generic Mapping Tools software [31] and the software for viewing 3D velocity structures beneath whole Japan Islands [32]. This work was financially supported in part by Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT) and by the Council for Science, Technology and Innovation (CSTI) through the Cross-ministerial Strategic Innovation Promotion Program (SIP), entitled “Enhancement of societal resiliency against natural disasters” (Funding agency: Japan Science Technology Agency).
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\n\nPolicy last updated: 2018-09-11
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He also obtained an MSc in Molecular and Genetic Medicine, and a Ph.D. in Clinical Immunology and Human Genetics from the University of Sheffield, UK. He also completed a short-term fellowship in Pediatric Clinical Immunology and Bone Marrow Transplantation at Newcastle General Hospital, England. Dr. Rezaei is a Full Professor of Immunology and Vice Dean of International Affairs and Research, at the School of Medicine, Tehran University of Medical Sciences, and the co-founder and head of the Research Center for Immunodeficiencies. He is also the founding president of the Universal Scientific Education and Research Network (USERN). Dr. Rezaei has directed more than 100 research projects and has designed and participated in several international collaborative projects. He is an editor, editorial assistant, or editorial board member of more than forty international journals. He has edited more than 50 international books, presented more than 500 lectures/posters in congresses/meetings, and published more than 1,100 scientific papers in international journals.",institutionString:"Tehran University of Medical Sciences",institution:{name:"Tehran University of Medical Sciences",country:{name:"Iran"}}},{id:"180733",title:"Dr.",name:"Jean",middleName:null,surname:"Engohang-Ndong",slug:"jean-engohang-ndong",fullName:"Jean Engohang-Ndong",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/180733/images/system/180733.png",biography:"Dr. Jean Engohang-Ndong was born and raised in Gabon. After obtaining his Associate Degree of Science at the University of Science and Technology of Masuku, Gabon, he continued his education in France where he obtained his BS, MS, and Ph.D. in Medical Microbiology. He worked as a post-doctoral fellow at the Public Health Research Institute (PHRI), Newark, NJ for four years before accepting a three-year faculty position at Brigham Young University-Hawaii. Dr. Engohang-Ndong is a tenured faculty member with the academic rank of Full Professor at Kent State University, Ohio, where he teaches a wide range of biological science courses and pursues his research in medical and environmental microbiology. Recently, he expanded his research interest to epidemiology and biostatistics of chronic diseases in Gabon.",institutionString:"Kent State University",institution:{name:"Kent State University",country:{name:"United States of America"}}},{id:"188773",title:"Prof.",name:"Emmanuel",middleName:null,surname:"Drouet",slug:"emmanuel-drouet",fullName:"Emmanuel Drouet",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/188773/images/system/188773.png",biography:"Emmanuel Drouet, PharmD, is a Professor of Virology at the Faculty of Pharmacy, the University Grenoble-Alpes, France. As a head scientist at the Institute of Structural Biology in Grenoble, Dr. Drouet’s research investigates persisting viruses in humans (RNA and DNA viruses) and the balance with our host immune system. He focuses on these viruses’ effects on humans (both their impact on pathology and their symbiotic relationships in humans). He has an excellent track record in the herpesvirus field, and his group is engaged in clinical research in the field of Epstein-Barr virus diseases. He is the editor of the online Encyclopedia of Environment and he coordinates the Universal Health Coverage education program for the BioHealth Computing Schools of the European Institute of Science.",institutionString:null,institution:{name:"Grenoble Alpes University",country:{name:"France"}}},{id:"131400",title:"Prof.",name:"Alfonso J.",middleName:null,surname:"Rodriguez-Morales",slug:"alfonso-j.-rodriguez-morales",fullName:"Alfonso J. Rodriguez-Morales",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/131400/images/system/131400.png",biography:"Dr. Rodriguez-Morales is an expert in tropical and emerging diseases, particularly zoonotic and vector-borne diseases (especially arboviral diseases). He is the president of the Travel Medicine Committee of the Pan-American Infectious Diseases Association (API), as well as the president of the Colombian Association of Infectious Diseases (ACIN). He is a member of the Committee on Tropical Medicine, Zoonoses, and Travel Medicine of ACIN. He is a vice-president of the Latin American Society for Travel Medicine (SLAMVI) and a Member of the Council of the International Society for Infectious Diseases (ISID). Since 2014, he has been recognized as a Senior Researcher, at the Ministry of Science of Colombia. He is a professor at the Faculty of Medicine of the Fundacion Universitaria Autonoma de las Americas, in Pereira, Risaralda, Colombia. He is an External Professor, Master in Research on Tropical Medicine and International Health, Universitat de Barcelona, Spain. He is also a professor at the Master in Clinical Epidemiology and Biostatistics, Universidad Científica del Sur, Lima, Peru. In 2021 he has been awarded the “Raul Isturiz Award” Medal of the API. Also, in 2021, he was awarded with the “Jose Felix Patiño” Asclepius Staff Medal of the Colombian Medical College, due to his scientific contributions to COVID-19 during the pandemic. He is currently the Editor in Chief of the journal Travel Medicine and Infectious Diseases. His Scopus H index is 47 (Google Scholar H index, 68).",institutionString:"Institución Universitaria Visión de las Américas, Colombia",institution:null},{id:"332819",title:"Dr.",name:"Chukwudi Michael",middleName:"Michael",surname:"Egbuche",slug:"chukwudi-michael-egbuche",fullName:"Chukwudi Michael Egbuche",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/332819/images/14624_n.jpg",biography:"I an Dr. Chukwudi Michael Egbuche. I am a Senior Lecturer in the Department of Parasitology and Entomology, Nnamdi Azikiwe University, Awka.",institutionString:null,institution:{name:"Nnamdi Azikiwe University",country:{name:"Nigeria"}}},{id:"284232",title:"Mr.",name:"Nikunj",middleName:"U",surname:"Tandel",slug:"nikunj-tandel",fullName:"Nikunj Tandel",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/284232/images/8275_n.jpg",biography:'Mr. Nikunj Tandel has completed his Master\'s degree in Biotechnology from VIT University, India in the year of 2012. He is having 8 years of research experience especially in the field of malaria epidemiology, immunology, and nanoparticle-based drug delivery system against the infectious diseases, autoimmune disorders and cancer. He has worked for the NIH funded-International Center of Excellence in Malaria Research project "Center for the study of complex malaria in India (CSCMi)" in collaboration with New York University. The preliminary objectives of the study are to understand and develop the evidence-based tools and interventions for the control and prevention of malaria in different sites of the INDIA. Alongside, with the help of next-generation genomics study, the team has studied the antimalarial drug resistance in India. Further, he has extended his research in the development of Humanized mice for the study of liver-stage malaria and identification of molecular marker(s) for the Artemisinin resistance. At present, his research focuses on understanding the role of B cells in the activation of CD8+ T cells in malaria. Received the CSIR-SRF (Senior Research Fellow) award-2018, FIMSA (Federation of Immunological Societies of Asia-Oceania) Travel Bursary award to attend the IUIS-IIS-FIMSA Immunology course-2019',institutionString:"Nirma University",institution:{name:"Nirma University",country:{name:"India"}}},{id:"334383",title:"Ph.D.",name:"Simone",middleName:"Ulrich",surname:"Ulrich Picoli",slug:"simone-ulrich-picoli",fullName:"Simone Ulrich Picoli",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/334383/images/15919_n.jpg",biography:"Graduated in Pharmacy from Universidade Luterana do Brasil (1999), Master in Agricultural and Environmental Microbiology from Federal University of Rio Grande do Sul (2002), Specialization in Clinical Microbiology from Universidade de São Paulo, USP (2007) and PhD in Sciences in Gastroenterology and Hepatology (2012). She is currently an Adjunct Professor at Feevale University in Medicine and Biomedicine courses and a permanent professor of the Academic Master\\'s Degree in Virology. She has experience in the field of Microbiology, with an emphasis on Bacteriology, working mainly on the following topics: bacteriophages, bacterial resistance, clinical microbiology and food microbiology.",institutionString:null,institution:{name:"Universidade Feevale",country:{name:"Brazil"}}},{id:"229220",title:"Dr.",name:"Amjad",middleName:"Islam",surname:"Aqib",slug:"amjad-aqib",fullName:"Amjad Aqib",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/229220/images/system/229220.png",biography:"Dr. Amjad Islam Aqib obtained a DVM and MSc (Hons) from University of Agriculture Faisalabad (UAF), Pakistan, and a PhD from the University of Veterinary and Animal Sciences Lahore, Pakistan. Dr. Aqib joined the Department of Clinical Medicine and Surgery at UAF for one year as an assistant professor where he developed a research laboratory designated for pathogenic bacteria. Since 2018, he has been Assistant Professor/Officer in-charge, Department of Medicine, Manager Research Operations and Development-ORIC, and President One Health Club at Cholistan University of Veterinary and Animal Sciences, Bahawalpur, Pakistan. He has nearly 100 publications to his credit. His research interests include epidemiological patterns and molecular analysis of antimicrobial resistance and modulation and vaccine development against animal pathogens of public health concern.",institutionString:"Cholistan University of Veterinary and Animal Sciences",institution:null},{id:"62900",title:"Prof.",name:"Fethi",middleName:null,surname:"Derbel",slug:"fethi-derbel",fullName:"Fethi Derbel",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/62900/images/system/62900.jpeg",biography:"Professor Fethi Derbel was born in 1960 in Tunisia. He received his medical degree from the Sousse Faculty of Medicine at Sousse, University of Sousse, Tunisia. He completed his surgical residency in General Surgery at the University Hospital Farhat Hached of Sousse and was a member of the Unit of Liver Transplantation in the University of Rennes, France. He then worked in the Department of Surgery at the Sahloul University Hospital in Sousse. Professor Derbel is presently working at the Clinique les Oliviers, Sousse, Tunisia. His hospital activities are mostly concerned with laparoscopic, colorectal, pancreatic, hepatobiliary, and gastric surgery. He is also very interested in hernia surgery and performs ventral hernia repairs and inguinal hernia repairs. He has been a member of the GREPA and Tunisian Hernia Society (THS). During his residency, he managed patients suffering from diabetic foot, and he was very interested in this pathology. For this reason, he decided to coordinate a book project dealing with the diabetic foot. Professor Derbel has published many articles in journals and collaborates intensively with IntechOpen Access Publisher as an editor.",institutionString:"Clinique les Oliviers",institution:null},{id:"300144",title:"Dr.",name:"Meriem",middleName:null,surname:"Braiki",slug:"meriem-braiki",fullName:"Meriem Braiki",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/300144/images/system/300144.jpg",biography:"Dr. Meriem Braiki is a specialist in pediatric surgeon from Tunisia. She was born in 1985. She received her medical degree from the University of Medicine at Sousse, Tunisia. She achieved her surgical residency training periods in Pediatric Surgery departments at University Hospitals in Monastir, Tunis and France.\r\nShe is currently working at the Pediatric surgery department, Sidi Bouzid Hospital, Tunisia. Her hospital activities are mostly concerned with laparoscopic, parietal, urological and digestive surgery. She has published several articles in diffrent journals.",institutionString:"Sidi Bouzid Regional Hospital",institution:null},{id:"229481",title:"Dr.",name:"Erika M.",middleName:"Martins",surname:"de Carvalho",slug:"erika-m.-de-carvalho",fullName:"Erika M. de Carvalho",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/229481/images/6397_n.jpg",biography:null,institutionString:null,institution:{name:"Oswaldo Cruz Foundation",country:{name:"Brazil"}}},{id:"186537",title:"Prof.",name:"Tonay",middleName:null,surname:"Inceboz",slug:"tonay-inceboz",fullName:"Tonay Inceboz",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/186537/images/system/186537.jfif",biography:"I was graduated from Ege University of Medical Faculty (Turkey) in 1988 and completed his Med. PhD degree in Medical Parasitology at the same university. I became an Associate Professor in 2008 and Professor in 2014. I am currently working as a Professor at the Department of Medical Parasitology at Dokuz Eylul University, Izmir, Turkey.\n\nI have given many lectures, presentations in different academic meetings. I have more than 60 articles in peer-reviewed journals, 18 book chapters, 1 book editorship.\n\nMy research interests are Echinococcus granulosus, Echinococcus multilocularis (diagnosis, life cycle, in vitro and in vivo cultivation), and Trichomonas vaginalis (diagnosis, PCR, and in vitro cultivation).",institutionString:"Dokuz Eylül University",institution:{name:"Dokuz Eylül University",country:{name:"Turkey"}}},{id:"71812",title:"Prof.",name:"Hanem Fathy",middleName:"Fathy",surname:"Khater",slug:"hanem-fathy-khater",fullName:"Hanem Fathy Khater",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/71812/images/1167_n.jpg",biography:"Prof. Khater is a Professor of Parasitology at Benha University, Egypt. She studied for her doctoral degree, at the Department of Entomology, College of Agriculture, Food and Natural Resources, University of Missouri, Columbia, USA. She has completed her Ph.D. degrees in Parasitology in Egypt, from where she got the award for “the best scientific Ph.D. dissertation”. She worked at the School of Biological Sciences, Bristol, England, the UK in controlling insects of medical and veterinary importance as a grant from Newton Mosharafa, the British Council. Her research is focused on searching of pesticides against mosquitoes, house flies, lice, green bottle fly, camel nasal botfly, soft and hard ticks, mites, and the diamondback moth as well as control of several parasites using safe and natural materials to avoid drug resistances and environmental contamination.",institutionString:null,institution:{name:"Banha University",country:{name:"Egypt"}}},{id:"99780",title:"Prof.",name:"Omolade",middleName:"Olayinka",surname:"Okwa",slug:"omolade-okwa",fullName:"Omolade Okwa",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/99780/images/system/99780.jpg",biography:"Omolade Olayinka Okwa is presently a Professor of Parasitology at Lagos State University, Nigeria. She has a PhD in Parasitology (1997), an MSc in Cellular Parasitology (1992), and a BSc (Hons) Zoology (1990) all from the University of Ibadan, Nigeria. She teaches parasitology at the undergraduate and postgraduate levels. She was a recipient of a Commonwealth fellowship supported by British Council tenable at the Centre for Entomology and Parasitology (CAEP), Keele University, United Kingdom between 2004 and 2005. She was awarded an Honorary Visiting Research Fellow at the same university from 2005 to 2007. \nShe has been an external examiner to the Department of Veterinary Microbiology and Parasitology, University of Ibadan, MSc programme between 2010 and 2012. She is a member of the Nigerian Society of Experimental Biology (NISEB), Parasitology and Public Health Society of Nigeria (PPSN), Science Association of Nigeria (SAN), Zoological Society of Nigeria (ZSN), and is Vice Chairperson of the Organisation of Women in Science (OWSG), LASU chapter. She served as Head of Department of Zoology and Environmental Biology, Lagos State University from 2007 to 2010 and 2014 to 2016. She is a reviewer for several local and international journals such as Unilag Journal of Science, Libyan Journal of Medicine, Journal of Medicine and Medical Sciences, and Annual Research and Review in Science. \nShe has authored 45 scientific research publications in local and international journals, 8 scientific reviews, 4 books, and 3 book chapters, which includes the books “Malaria Parasites” and “Malaria” which are IntechOpen access publications.",institutionString:"Lagos State University",institution:{name:"Lagos State University",country:{name:"Nigeria"}}},{id:"273100",title:"Dr.",name:"Vijay",middleName:null,surname:"Gayam",slug:"vijay-gayam",fullName:"Vijay Gayam",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/273100/images/system/273100.jpeg",biography:"Dr. Vijay Bhaskar Reddy Gayam is currently practicing as an internist at Interfaith Medical Center in Brooklyn, New York, USA. He is also a Clinical Assistant Professor at the SUNY Downstate University Hospital and Adjunct Professor of Medicine at the American University of Antigua. He is a holder of an M.B.B.S. degree bestowed to him by Osmania Medical College and received his M.D. at Interfaith Medical Center. His career goals thus far have heavily focused on direct patient care, medical education, and clinical research. He currently serves in two leadership capacities; Assistant Program Director of Medicine at Interfaith Medical Center and as a Councilor for the American\r\nFederation for Medical Research. As a true academician and researcher, he has more than 50 papers indexed in international peer-reviewed journals. He has also presented numerous papers in multiple national and international scientific conferences. His areas of research interest include general internal medicine, gastroenterology and hepatology. He serves as an editor, editorial board member and reviewer for multiple international journals. His research on Hepatitis C has been very successful and has led to multiple research awards, including the 'Equity in Prevention and Treatment Award” from the New York Department of Health Viral Hepatitis Symposium (2018) and the 'Presidential Poster Award” awarded to him by the American College of Gastroenterology (2018). He was also awarded 'Outstanding Clinician in General Medicine” by Venus International Foundation for his extensive research expertise and services, perform over and above the standard expected in the advancement of healthcare, patient safety and quality of care.",institutionString:"Interfaith Medical Center",institution:{name:"Interfaith Medical Center",country:{name:"United States of America"}}},{id:"93517",title:"Dr.",name:"Clement",middleName:"Adebajo",surname:"Meseko",slug:"clement-meseko",fullName:"Clement Meseko",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/93517/images/system/93517.jpg",biography:"Dr. Clement Meseko obtained DVM and PhD degree in Veterinary Medicine and Virology respectively. He has worked for over 20 years in both private and public sectors including the academia, contributing to knowledge and control of infectious disease. Through the application of epidemiological skill, classical and molecular virological skills, he investigates viruses of economic and public health importance for the mitigation of the negative impact on people, animal and the environment in the context of Onehealth. \r\nDr. Meseko’s field experience on animal and zoonotic diseases and pathogen dynamics at the human-animal interface over the years shaped his carrier in research and scientific inquiries. He has been part of the investigation of Highly Pathogenic Avian Influenza incursions in sub Saharan Africa and monitors swine Influenza (Pandemic influenza Virus) agro-ecology and potential for interspecies transmission. He has authored and reviewed a number of journal articles and book chapters.",institutionString:"National Veterinary Research Institute",institution:{name:"National Veterinary Research Institute",country:{name:"Nigeria"}}},{id:"158026",title:"Prof.",name:"Shailendra K.",middleName:null,surname:"Saxena",slug:"shailendra-k.-saxena",fullName:"Shailendra K. Saxena",position:null,profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRET3QAO/Profile_Picture_2022-05-10T10:10:26.jpeg",biography:"Professor Dr. Shailendra K. Saxena is a vice dean and professor at King George's Medical University, Lucknow, India. His research interests involve understanding the molecular mechanisms of host defense during human viral infections and developing new predictive, preventive, and therapeutic strategies for them using Japanese encephalitis virus (JEV), HIV, and emerging viruses as a model via stem cell and cell culture technologies. 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Many parasitic diseases are classified as neglected tropical diseases because they have received minimal funding over recent years and, in many cases, are under-reported despite the critical role they play in morbidity and mortality among human and animal hosts. The current topic, Parasitic Infectious Diseases, in the Infectious Diseases Series aims to publish studies on the systematics, epidemiology, molecular biology, genomics, pathogenesis, genetics, and clinical significance of parasitic diseases from blood borne to intestinal parasites as well as zoonotic parasites. We hope to cover all aspects of parasitic diseases to provide current and relevant research data on these very important diseases. In the current atmosphere of the Coronavirus pandemic, communities around the world, particularly those in different underdeveloped areas, are faced with the growing challenges of the high burden of parasitic diseases. At the same time, they are faced with the Covid-19 pandemic leading to what some authors have called potential syndemics that might worsen the outcome of such infections. Therefore, it is important to conduct studies that examine parasitic infections in the context of the coronavirus pandemic for the benefit of all communities to help foster more informed decisions for the betterment of human and animal health.",coverUrl:"https://cdn.intechopen.com/series_topics/covers/5.jpg",keywords:"Blood Borne Parasites, Intestinal Parasites, Protozoa, Helminths, Arthropods, Water Born Parasites, Epidemiology, Molecular Biology, Systematics, Genomics, Proteomics, Ecology"},{id:"6",title:"Viral Infectious Diseases",scope:"The Viral Infectious Diseases Book Series aims to provide a comprehensive overview of recent research trends and discoveries in various viral infectious diseases emerging around the globe. The emergence of any viral disease is hard to anticipate, which often contributes to death. A viral disease can be defined as an infectious disease that has recently appeared within a population or exists in nature with the rapid expansion of incident or geographic range. This series will focus on various crucial factors related to emerging viral infectious diseases, including epidemiology, pathogenesis, host immune response, clinical manifestations, diagnosis, treatment, and clinical recommendations for managing viral infectious diseases, highlighting the recent issues with future directions for effective therapeutic strategies.",coverUrl:"https://cdn.intechopen.com/series_topics/covers/6.jpg",keywords:"Novel Viruses, Virus Transmission, Virus Evolution, Molecular Virology, Control and Prevention, Virus-host Interaction"}],annualVolumeBook:{},thematicCollection:[{type:"book",id:"11672",title:"Chemokines Updates",subtitle:null,isOpenForSubmission:!0,hash:"c00855833476a514d37abf7c846e16e9",slug:null,bookSignature:"Prof. Murat Şentürk",coverURL:"https://cdn.intechopen.com/books/images_new/11672.jpg",editedByType:null,submissionDeadline:"May 6th 2022",editors:[{id:"14794",title:"Prof.",name:"Murat",middleName:null,surname:"Şentürk",slug:"murat-senturk",fullName:"Murat Şentürk",profilePictureURL:"https://mts.intechopen.com/storage/users/14794/images/system/14794.jpeg",biography:"Dr. Murat Şentürk obtained a baccalaureate degree in Chemistry in 2002, a master’s degree in Biochemistry in 2006, and a doctorate degree in Biochemistry in 2009 from Atatürk University, Turkey. Dr. Şentürk currently works as an professor of Biochemistry in the Department of Basic Pharmacy Sciences, Faculty of Pharmacy, Ağri Ibrahim Cecen University, Turkey. \nDr. Şentürk published over 120 scientific papers, reviews, and book chapters and presented several conferences to scientists. \nHis research interests span enzyme inhibitor or activator, protein expression, purification and characterization, drug design and synthesis, toxicology, and pharmacology. \nHis research work has focused on neurodegenerative diseases and cancer treatment. Dr. Şentürk serves as the editorial board member of several international journals.",institutionString:"Ağrı İbrahim Çeçen University",position:null,outsideEditionCount:0,totalCites:0,totalAuthoredChapters:"2",totalChapterViews:"0",totalEditedBooks:"1",institution:{name:"Ağrı İbrahim Çeçen University",institutionURL:null,country:{name:"Turkey"}}}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null}],selectedSeries:null,selectedSubseries:null},seriesLanding:{item:{id:"11",title:"Biochemistry",doi:"10.5772/intechopen.72877",issn:"2632-0983",scope:"Biochemistry, the study of chemical transformations occurring within living organisms, impacts all areas of life sciences, from molecular crystallography and genetics to ecology, medicine, and population biology. Biochemistry examines macromolecules - proteins, nucleic acids, carbohydrates, and lipids – and their building blocks, structures, functions, and interactions. Much of biochemistry is devoted to enzymes, proteins that catalyze chemical reactions, enzyme structures, mechanisms of action and their roles within cells. Biochemistry also studies small signaling molecules, coenzymes, inhibitors, vitamins, and hormones, which play roles in life processes. Biochemical experimentation, besides coopting classical chemistry methods, e.g., chromatography, adopted new techniques, e.g., X-ray diffraction, electron microscopy, NMR, radioisotopes, and developed sophisticated microbial genetic tools, e.g., auxotroph mutants and their revertants, fermentation, etc. More recently, biochemistry embraced the ‘big data’ omics systems. Initial biochemical studies have been exclusively analytic: dissecting, purifying, and examining individual components of a biological system; in the apt words of Efraim Racker (1913 –1991), “Don’t waste clean thinking on dirty enzymes.” Today, however, biochemistry is becoming more agglomerative and comprehensive, setting out to integrate and describe entirely particular biological systems. The ‘big data’ metabolomics can define the complement of small molecules, e.g., in a soil or biofilm sample; proteomics can distinguish all the comprising proteins, e.g., serum; metagenomics can identify all the genes in a complex environment, e.g., the bovine rumen. This Biochemistry Series will address the current research on biomolecules and the emerging trends with great promise.",coverUrl:"https://cdn.intechopen.com/series/covers/11.jpg",latestPublicationDate:"July 5th, 2022",hasOnlineFirst:!0,numberOfOpenTopics:4,numberOfPublishedChapters:320,numberOfPublishedBooks:32,editor:{id:"31610",title:"Dr.",name:"Miroslav",middleName:null,surname:"Blumenberg",fullName:"Miroslav Blumenberg",profilePictureURL:"https://mts.intechopen.com/storage/users/31610/images/system/31610.jpg",biography:"Miroslav Blumenberg, Ph.D., was born in Subotica and received his BSc in Belgrade, Yugoslavia. He completed his Ph.D. at MIT in Organic Chemistry; he followed up his Ph.D. with two postdoctoral study periods at Stanford University. Since 1983, he has been a faculty member of the RO Perelman Department of Dermatology, NYU School of Medicine, where he is codirector of a training grant in cutaneous biology. Dr. Blumenberg’s research is focused on the epidermis, expression of keratin genes, transcription profiling, keratinocyte differentiation, inflammatory diseases and cancers, and most recently the effects of the microbiome on the skin. He has published more than 100 peer-reviewed research articles and graduated numerous Ph.D. and postdoctoral students.",institutionString:null,institution:{name:"New York University Langone Medical Center",institutionURL:null,country:{name:"United States of America"}}},subseries:[{id:"14",title:"Cell and Molecular Biology",keywords:"Omics (Transcriptomics; Proteomics; Metabolomics), Molecular Biology, Cell Biology, Signal Transduction and Regulation, Cell Growth and Differentiation, Apoptosis, Necroptosis, Ferroptosis, Autophagy, Cell Cycle, Macromolecules and Complexes, Gene Expression",scope:"The Cell and Molecular Biology topic within the IntechOpen Biochemistry Series aims to rapidly publish contributions on all aspects of cell and molecular biology, including aspects related to biochemical and genetic research (not only in humans but all living beings). We encourage the submission of manuscripts that provide novel and mechanistic insights that report significant advances in the fields. Topics include, but are not limited to: Advanced techniques of cellular and molecular biology (Molecular methodologies, imaging techniques, and bioinformatics); Biological activities at the molecular level; Biological processes of cell functions, cell division, senescence, maintenance, and cell death; Biomolecules interactions; Cancer; Cell biology; Chemical biology; Computational biology; Cytochemistry; Developmental biology; Disease mechanisms and therapeutics; DNA, and RNA metabolism; Gene functions, genetics, and genomics; Genetics; Immunology; Medical microbiology; Molecular biology; Molecular genetics; Molecular processes of cell and organelle dynamics; Neuroscience; Protein biosynthesis, degradation, and functions; Regulation of molecular interactions in a cell; Signalling networks and system biology; Structural biology; Virology and microbiology.",annualVolume:11410,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/14.jpg",editor:{id:"165627",title:"Dr.",name:"Rosa María",middleName:null,surname:"Martínez-Espinosa",fullName:"Rosa María Martínez-Espinosa",profilePictureURL:"https://mts.intechopen.com/storage/users/165627/images/system/165627.jpeg",institutionString:null,institution:{name:"University of Alicante",institutionURL:null,country:{name:"Spain"}}},editorTwo:null,editorThree:null,editorialBoard:[{id:"79367",title:"Dr.",name:"Ana Isabel",middleName:null,surname:"Flores",fullName:"Ana Isabel Flores",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRpIOQA0/Profile_Picture_1632418099564",institutionString:null,institution:{name:"Hospital Universitario 12 De Octubre",institutionURL:null,country:{name:"Spain"}}},{id:"328234",title:"Ph.D.",name:"Christian",middleName:null,surname:"Palavecino",fullName:"Christian Palavecino",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y000030DhEhQAK/Profile_Picture_1628835318625",institutionString:null,institution:{name:"Central University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"186585",title:"Dr.",name:"Francisco Javier",middleName:null,surname:"Martin-Romero",fullName:"Francisco Javier Martin-Romero",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSB3HQAW/Profile_Picture_1631258137641",institutionString:null,institution:{name:"University of Extremadura",institutionURL:null,country:{name:"Spain"}}}]},{id:"15",title:"Chemical Biology",keywords:"Phenolic Compounds, Essential Oils, Modification of Biomolecules, Glycobiology, Combinatorial Chemistry, Therapeutic peptides, Enzyme Inhibitors",scope:"Chemical biology spans the fields of chemistry and biology involving the application of biological and chemical molecules and techniques. In recent years, the application of chemistry to biological molecules has gained significant interest in medicinal and pharmacological studies. This topic will be devoted to understanding the interplay between biomolecules and chemical compounds, their structure and function, and their potential applications in related fields. Being a part of the biochemistry discipline, the ideas and concepts that have emerged from Chemical Biology have affected other related areas. This topic will closely deal with all emerging trends in this discipline.",annualVolume:11411,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/15.jpg",editor:{id:"441442",title:"Dr.",name:"Şükrü",middleName:null,surname:"Beydemir",fullName:"Şükrü Beydemir",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y00003GsUoIQAV/Profile_Picture_1634557147521",institutionString:null,institution:{name:"Anadolu University",institutionURL:null,country:{name:"Turkey"}}},editorTwo:{id:"13652",title:"Prof.",name:"Deniz",middleName:null,surname:"Ekinci",fullName:"Deniz Ekinci",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002aYLT1QAO/Profile_Picture_1634557223079",institutionString:null,institution:{name:"Ondokuz Mayıs University",institutionURL:null,country:{name:"Turkey"}}},editorThree:null,editorialBoard:[{id:"219081",title:"Dr.",name:"Abdulsamed",middleName:null,surname:"Kükürt",fullName:"Abdulsamed Kükürt",profilePictureURL:"https://mts.intechopen.com/storage/users/219081/images/system/219081.png",institutionString:null,institution:{name:"Kafkas University",institutionURL:null,country:{name:"Turkey"}}},{id:"241413",title:"Dr.",name:"Azhar",middleName:null,surname:"Rasul",fullName:"Azhar Rasul",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRT1oQAG/Profile_Picture_1635251978933",institutionString:null,institution:{name:"Government College University, Faisalabad",institutionURL:null,country:{name:"Pakistan"}}},{id:"178316",title:"Ph.D.",name:"Sergey",middleName:null,surname:"Sedykh",fullName:"Sergey Sedykh",profilePictureURL:"https://mts.intechopen.com/storage/users/178316/images/system/178316.jfif",institutionString:null,institution:{name:"Novosibirsk State University",institutionURL:null,country:{name:"Russia"}}}]},{id:"17",title:"Metabolism",keywords:"Biomolecules Metabolism, Energy Metabolism, Metabolic Pathways, Key Metabolic Enzymes, Metabolic Adaptation",scope:"Metabolism is frequently defined in biochemistry textbooks as the overall process that allows living systems to acquire and use the free energy they need for their vital functions or the chemical processes that occur within a living organism to maintain life. Behind these definitions are hidden all the aspects of normal and pathological functioning of all processes that the topic ‘Metabolism’ will cover within the Biochemistry Series. Thus all studies on metabolism will be considered for publication.",annualVolume:11413,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/17.jpg",editor:{id:"138626",title:"Dr.",name:"Yannis",middleName:null,surname:"Karamanos",fullName:"Yannis Karamanos",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002g6Jv2QAE/Profile_Picture_1629356660984",institutionString:null,institution:{name:"Artois University",institutionURL:null,country:{name:"France"}}},editorTwo:null,editorThree:null,editorialBoard:[{id:"243049",title:"Dr.",name:"Anca",middleName:null,surname:"Pantea Stoian",fullName:"Anca Pantea Stoian",profilePictureURL:"https://mts.intechopen.com/storage/users/243049/images/system/243049.jpg",institutionString:null,institution:{name:"Carol Davila University of Medicine and Pharmacy",institutionURL:null,country:{name:"Romania"}}},{id:"203824",title:"Dr.",name:"Attilio",middleName:null,surname:"Rigotti",fullName:"Attilio Rigotti",profilePictureURL:"//cdnintech.com/web/frontend/www/assets/author.svg",institutionString:null,institution:{name:"Pontifical Catholic University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"300470",title:"Dr.",name:"Yanfei (Jacob)",middleName:null,surname:"Qi",fullName:"Yanfei (Jacob) Qi",profilePictureURL:"https://mts.intechopen.com/storage/users/300470/images/system/300470.jpg",institutionString:null,institution:{name:"Centenary Institute of Cancer Medicine and Cell Biology",institutionURL:null,country:{name:"Australia"}}}]},{id:"18",title:"Proteomics",keywords:"Mono- and Two-Dimensional Gel Electrophoresis (1-and 2-DE), Liquid Chromatography (LC), Mass Spectrometry/Tandem Mass Spectrometry (MS; MS/MS), Proteins",scope:"With the recognition that the human genome cannot provide answers to the etiology of a disorder, changes in the proteins expressed by a genome became a focus in research. Thus proteomics, an area of research that detects all protein forms expressed in an organism, including splice isoforms and post-translational modifications, is more suitable than genomics for a comprehensive understanding of the biochemical processes that govern life. The most common proteomics applications are currently in the clinical field for the identification, in a variety of biological matrices, of biomarkers for diagnosis and therapeutic intervention of disorders. From the comparison of proteomic profiles of control and disease or different physiological states, which may emerge, changes in protein expression can provide new insights into the roles played by some proteins in human pathologies. Understanding how proteins function and interact with each other is another goal of proteomics that makes this approach even more intriguing. Specialized technology and expertise are required to assess the proteome of any biological sample. Currently, proteomics relies mainly on mass spectrometry (MS) combined with electrophoretic (1 or 2-DE-MS) and/or chromatographic techniques (LC-MS/MS). MS is an excellent tool that has gained popularity in proteomics because of its ability to gather a complex body of information such as cataloging protein expression, identifying protein modification sites, and defining protein interactions. The Proteomics topic aims to attract contributions on all aspects of MS-based proteomics that, by pushing the boundaries of MS capabilities, may address biological problems that have not been resolved yet.",annualVolume:11414,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/18.jpg",editor:{id:"200689",title:"Prof.",name:"Paolo",middleName:null,surname:"Iadarola",fullName:"Paolo Iadarola",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSCl8QAG/Profile_Picture_1623568118342",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorTwo:{id:"201414",title:"Dr.",name:"Simona",middleName:null,surname:"Viglio",fullName:"Simona Viglio",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRKDHQA4/Profile_Picture_1630402531487",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorThree:null,editorialBoard:[{id:"72288",title:"Dr.",name:"Arli Aditya",middleName:null,surname:"Parikesit",fullName:"Arli Aditya Parikesit",profilePictureURL:"https://mts.intechopen.com/storage/users/72288/images/system/72288.jpg",institutionString:null,institution:{name:"Indonesia International Institute for Life Sciences",institutionURL:null,country:{name:"Indonesia"}}},{id:"40928",title:"Dr.",name:"Cesar",middleName:null,surname:"Lopez-Camarillo",fullName:"Cesar Lopez-Camarillo",profilePictureURL:"https://mts.intechopen.com/storage/users/40928/images/3884_n.png",institutionString:null,institution:{name:"Universidad Autónoma de la Ciudad de México",institutionURL:null,country:{name:"Mexico"}}},{id:"81926",title:"Dr.",name:"Shymaa",middleName:null,surname:"Enany",fullName:"Shymaa Enany",profilePictureURL:"https://mts.intechopen.com/storage/users/81926/images/system/81926.png",institutionString:"Suez Canal University",institution:{name:"Suez Canal University",institutionURL:null,country:{name:"Egypt"}}}]}]}},libraryRecommendation:{success:null,errors:{},institutions:[]},route:{name:"chapter.detail",path:"/chapters/29726",hash:"",query:{},params:{id:"29726"},fullPath:"/chapters/29726",meta:{},from:{name:null,path:"/",hash:"",query:{},params:{},fullPath:"/",meta:{}}}},function(){var e;(e=document.currentScript||document.scripts[document.scripts.length-1]).parentNode.removeChild(e)}()