Classification of the Mount Bambouto caldera in the CCDB of [10].
\r\n\t
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Trigeminal nerves mediate orofacial somatosensory sensations, including dental orofacial pain. The primary trigeminal ganglia nociceptive neurons send axonal fibers innervating orofacial tissues as well as forming synapses with secondary nociceptive neurons in the brainstem. Noxious stimuli, biological insults, or pain mediators released following tissue injury and inflammations activate the nociceptors resulting in the nociceptive transduction in peripheral sensory nerves. The pain signal is conducted and further transmitted to the secondary and higher level nociceptive neurons via synaptic transmission in the brain. Nociception also depends on the condition and status of the sensory nervous system. Pain signal processing can be facilitated with maladaptive plasticity or neuropathy changes in the nociceptive pathway that result in pain sensitization or neuropathic pain. These changes include nociceptive sensitization, malfunctioned inhibition, and circuit-level rewiring/aberrant processing [1] in both the peripheral and central nociceptive nerves. As peripheral or central sensitization occurs, slight noxious stimulation or even non-noxious stimulation induces severe pain, a phenomenon that is called hyperalgesia or allodynia, respectively. In sensitization condition, patients may also present with spontaneous and neuropathic pain without apparent stimulus. In contrast to the pain from extra-orofacial regions, dental orofacial pain is usually accompanied by the presence of hyperalgesia, allodynia. Dental orofacial pain patients often experience more severe pain and are typically emotional-distracted. Besides, patients with dental orofacial pain are prone to develop spontaneous pain, referred pain, and neuropathic pain [2].
For the past decades, studies strongly suggest a key modulatory role of purinergic signaling in pain generation and sensitization in the nociceptive nerves [3, 4, 5, 6, 7]. ATP induces pain via activation of P2X receptors in peripheral sensory nerve fibers. ATP is also involved in cross-talk between the primary and secondary nociceptive neurons as well as with astrocytes and microglia. Since ATP and its metabolites are pain mediators and participate in pain signal processing via activation of various purinergic receptors (P1 and P2 receptors) in the nociceptive sensory nerves [5, 8, 9, 10], one putative explanation for the unique properties in dental orofacial pain is due to the different existence or expression of purinergic signaling in trigeminal nerves. Indeed, it has been observed that purinergic receptors are preferentially expressed in trigeminal nociceptive neurons compared with that in dorsal root ganglions [11, 12]. Purinergic signaling depends on ATP release, purinergic receptors (P1, P2X, and P2Y) activation, and extracellular enzymatic ATP degradation and adenosine generation. Therefore, identification of the machinery components for purinergic signaling in the trigeminal nociceptive pathway will provide promising insight to understand the underlying nociceptive mechanisms for the pathogenesis of dental orofacial pain.
In this chapter, we overview the expression of purinergic receptors and machinery for ATP release, ATP degradation, adenosine generation in the trigeminal nociceptive nerves, and discuss the role of purinergic signaling in the pathogenesis of dentin hypersensitivity and dental orofacial pain. Understanding the role of purinergic signaling in the nociceptive mechanisms for pain signal transduction, transmission, sensitization, and modulation in trigeminal nerves will reveal multiple targets for developing more effective drugs and therapies for the management of dental orofacial pain.
ATP has been recognized as a neuronal transmitter and modulator in synaptic transmission for decades [13]. ATP and its metabolites are also important pain mediators and modulators in pain signal processing [5, 8, 9, 10]. It has been proposed that ATP released from various cell types is implicated in initiating the pain signal by acting on purinoceptors on sensory nerve terminals [14]. Purinoreceptors responsible for pain transduction belong to P2X receptor family, a group of ligand-gated non-selective cation channels using ATP as a native agonist. Upon binding to P2X receptors, ATP opens the pore of channels permeable to Na+, K+, and Ca2+ that depolarize the membrane potential, enhance the excitability and induce spikes in nociceptive neurons. So far, seven distinct P2X receptor subunits (P2X1–P2X7) have been isolated and cloned (North 2002). A total of 14 functional homo- or heterotrimers P2X receptors (P2X1–P2X7, P2X1/2, P2X1/4, P2X1/5, P2X2/3, P2X2/6, P2X4/6, and possibly P2X4/7) assembled from different subunits had been reported [15].
Using in situ hybridization immunohistochemistry (ISHH), mRNA expression for P2X2, 3, 4, 5, and 6 receptors had been detected in naive dorsal root ganglia (DRG) neurons, in which P2X2 and P2X3 receptors were expressed preferentially by C-fiber neurons. In contrast, the majority of P2X5 and P2X6 receptors were preferentially expressed by A-fiber neurons [16]. Specifically, expression of P2X receptors is also detected in nociceptive primary sensory neurons, peripheral nociceptive nerve fibers, and their free endings extending throughout the epidermis. Two types of P2X receptors (P2X2 and P2X3) have been particularly examined in DRG presumably nociceptive neurons [17]. P2X3 receptors appear to be exclusively expressed in a subgroup of sensory neurons that are likely to be nociceptive neurons [18]. Nociceptive neurons fall into nerve growth factor (NGF) sensitive group and glial cell-line derived neurotrophic factor (GDNF) sensitive group. It turned out that the vast majority of P2X3 positive neurons overlap with GDNF subgroup of nociceptive neurons [19]. P2X3 receptors are peripherally axonal transported and have been identified in the free end of the nerve fibers in a variety of tissues including tongue, skin, and viscera (e.g., bladder) [17, 19]. Co-localization studies suggest that many, but not all, DRG cells that express P2X2 receptors also express P2X3 receptors [17]. Furthermore, electrophysiological and pharmacological studies had demonstrated that the application of ATP or its analogs to DRG neurons results in depolarization or inward currents mediated by P2X receptors activation.
The selective expression of P2X3 and P2X2 receptors within the nociceptive nerves has inspired a variety of approaches to elucidate the potential role of ATP as a pain mediator. ATP elicits excitatory inward currents in nociceptive small diameter sensory ganglion cells. Interestingly, these inward currents resemble the currents evoked by ATP on recombinantly expressed heteromeric P2X(2/3) channels as well as homomultimers consisting of P2X2 and P2X3 [8, 14, 18, 20]. It had been observed that ATP and its analogs produce spike activity when applied to peripheral nociceptive terminals [8]. In in vivo pain behavioral animal models, the algogenic effects of ATP in normal conditions and models of peripheral sensitization had been confirmed. In humans, local skin delivery of ATP induces dosage-dependent pain sensation. Furthermore, it has been shown that ATP-induced algogenic responses depends on capsaicin-sensitive neurons and is augmented in the presence of inflammatory mediators. Since ATP is released in the vicinity of peripheral nociceptive terminals under a variety of conditions such as tissue injury or inflammation, the existence of purinergic signaling in peripheral sensory nervous free ends strongly links the tissue damage and inflammation to pain perception [9].
Noxious stimulation to the nociceptive nerves induces pain sensation in the brain. Acute pain is a warning signal for the individual to survive in response to tissue injuries or diseases. However, in nociceptive sensitization statuses, such as in chronic pain or neuropathic pain, nociception no longer relates to or depends on external noxious stimulation, and slight noxious or even no-noxious stimulation or non-stimulation at all can induce severe pain. The central sensitization theory proposed that neuronal plasticity occurred in the sensory nerve circuits that enhance the sensitivity to noxious stimuli or even turn the innocuous slight touching to pain [21]. Pain sensitization can also be induced by nerve injury (deafferentation, compression, and constriction) or neuropathy changes resulting from physical, chemical, metabolic, or biological insults to the sensory nerves. Besides, it has been proposed the pain signal itself that is accompanied with releasing of proinflammatory cytokines, neuronal transmitters, and modulators in nociceptive neuronal circuits participate in plasticity changes and induce central sensitization [22].
Synaptic neuronal transmission is accompanied with large amount of ATP release. Accumulated evidence suggests that ATP signaling play an essential role in the development and maintenance of central sensitization (Figure 1) [3, 4, 5, 6, 7]. In the somatosensory nerves, P2X receptors are expressed in DRG nociceptive neurons and then transferred to central axonal terminals as well as peripheral free ends. For example, immunoreactivity to P2X3 subunits is detected in lamina IIi in spinal cord dorsal horn and is disappeared after axotomy or following destruction of IB4-positive afferent fibers [17]. Immunoreactivity to P2X1 and P2X2 subunits are also located on the central terminals of primary afferent neurons that innervate superficial lamina of the spinal cord dorsal horn [17]. The presence of P2X receptor subunits at the central terminals of primary afferent neurons raises the possibility that ATP may act on central terminals of primary afferent neurons to either modulate or directly evoke the release of neuronal transmitters such as glutamate and neuropeptides. Activation of central terminal P2X receptors will depolarize the membrane potential and induce Ca2+ influx that will enhance the release of glutamate and substance P, and subsequently increase the secondary nociceptive neuron responses and dorsal horn nociceptive output. In neuropathic pain condition, an increase in the number of P2X receptors positive DRG neurons is observed following sciatic nerve injury by chronic constriction [23]. Specifically, an increase of P2X3 receptor immunoreactivity is detected in the dorsal horn ipsilateral side of the injured nerve indicating the upregulation of P2X receptors at the central terminals of primary afferent neurons. P2X receptor expression is also upregulated following tissue injury or inflammation within the spinal cord. The upregulation of P2X receptor expression on the central terminals of primary afferent neurons would sensitize the responses to ATP, which in turn may facilitate P2X receptor-mediated nociceptive modulation.
Activation of homomeric, as well as heteromeric P2X2/3 receptors, appears to modulate longer lasting nociceptive sensation associated with nerve injury or chronic inflammation [1]. P2X3 receptor function is highly sensitive to soluble factors like neuropeptides and neurotrophins and is controlled by transduction mechanisms, protein-protein interactions, and discrete membrane compartmentalization. Recent findings have demonstrated that P2X3 receptors interact with the synaptic scaffold protein calcium/calmodulin-dependent serine protein kinase (CASK) in a state-dependent fashion, indicating that CASK plays a crucial role in the modulation of P2X3 receptor stability and efficiency [24]. Activation of P2X3 receptors within CASK/P2X3 complex has essential consequences for neuronal plasticity and possibly for the release of neuromodulators and neurotransmitters. Better understanding the interaction machinery for P2X3 receptors and their integration with other receptors and channels on pre- and postsynaptic membranes is proposed to be essential to unveil the process of nociceptive neuronal sensitization.
Multiple other purinoceptor subtypes participate in pain processing. In neuropathic pain, activation of purinergic receptors on microglia is thought to maintain nociceptive sensitization through neural-glial cell interactions [3]. Microglia expresses several P2 receptor subtypes, and of these the P2X4, 7, and P2Y12 receptor subtypes have been implicated in neuropathic pain. It has been shown that activation of P2X4, 7, and P2Y12 receptors expressed on microglia is critically involved in neuropathic pain arising from peripheral nerve injury [25], while blocking these receptor with antagonists reduces neuropathic pain [3]. The P2X4 receptor has emerged as the core microglia-neuron signaling pathway. In response to peripheral nerve injury, P2X4 receptors are upregulated in spinal cord microglia [26]. Activation of this receptor causes the release of brain-derived neurotrophic factor (BDNF) which causes disinhibition of pain-transmission neurons in spinal lamina I. Several mechanisms have recently been implicated in the upregulation of P2X4 receptors including CCL21, interferon γ, tryptase, fibronectin, and the activation of μ-opioid receptors. Activation of P2X4 receptors leads to an influx of extracellular Ca2+ activating p38 MAPK that leads to SNARE-dependent release of BDNF from the microglia. BDNF is a crucial microglia-neuron signaling molecule that causes disinhibition of nociceptive dorsal horn neurons by disrupting intracellular Cl− homeostasis of inhibitory interneurons [27, 28, 29]. Activation of P2X7 or P2Y12 receptors is also through signals of p38 MAPK. p38 MAPK signaling drives the release of interleukin-1β and cathepsin S, which contributes to the maintenance of mechanical hypersensitivity in the spinal cord. P2Y12 receptor expression is also upregulated in microglia, and activation of these receptors is involved in neuropathic pain. Recent studies have demonstrated that inhibition of microglia-expressed P2 receptors (P2X4, P2X7 or P2Y12) by the pharmacological blockade, antisense knockdown or genetic deletion suppresses both mechanical allodynia and thermal hyperalgesia in nerve-injured rats [30, 31]. Conversely, intrathecal administration of the P2Y12 receptor agonist 2Me-SADP elicits pain behaviors in naïve rats that mimic those observed in nerve-injured rats [30].
In contrast to the algogenic effects of ATP, adenosine, the metabolite of ATP, induces antinociception via activation of P1 receptors. P1 receptors are G protein-coupled metabotropic receptors. Four subtypes of P1 receptors (A1, A2A, A2B, and A3) have been cloned in the nervous system [32].
A1 receptor is detected in the peripheral sensory nerve fibers [33]. Local delivery of adenosine induces analgesia and blocking A1 receptors abolishes adenosine-induced antinociception in various inflammatory pain models [34]. In addition, it has been shown that adenosine also mediates the analgesic mechanism of acupuncture via peripheral A1 receptors [35]. Adenosine also produces antinociception via activation of A1 receptors in the spinal cord [33]. Intraspinal injection of adenosine or A1 receptor agonists induced antinociception in both inflammatory and neuropathic pain animal models. It has been proposed that the underlying mechanism for adenosine-induced antinociception is related to potassium channel activation-induced cell membrane hyperpolarization [36]. Activation of pre- or postsynaptic A1 receptor triggers cAMP/PKA, PLC/IP3/DAG, and nitric oxide/cGMP/PKG pathways [33, 37] that induce analgesia by reducing presynaptic vesicle release and postsynaptic excitability [36]. Indeed, it has been demonstrated that A1 receptor activation decreased the excitatory neurotransmitter release in synaptosomes isolated from the spinal cord dorsal horns [38, 39].
Endogenous adenosine also mediates antinociception by A2A, A2B, or A3 receptors expressed in nociceptive neurons, astrocytes, or immune cells [40, 41]. Considering the extensive involvements of glial cells (microglia and astrocytes) in central sensitization and chronic pain [42], activation of adenosine receptors on microglia and astrocytes are potentially involved in the antinociceptive mechanism of adenosine in the nervous system [43]. Additionally, adenosine may also mediate the antinociception by enhancing GABA inhibition and blocking neuroinflammation via activation of A3 receptors [44]. Collectively, these studies suggest the possibility of treating chronic pain by targeting specific adenosine receptor subtypes in anatomically defined regions with agonists or with ecto-nucleotidases that control the generation of adenosine.
Purinergic signaling depends on ATP release, purinergic receptor action, and sequential hydrolysis of ATP to ADP and nucleoside adenosine [45]. Because of their dynamic catalytic activities under physiological conditions, ecto-nucleotide diphosphatases (Ecto-NTPDases) are the major enzymes responsible for the hydrolysis of extracellular ATP and ADP. Four members of ecto-NTPDse family (NTPDase1, 2, 3, and 8) have been cloned. Three of which (i.e., NTPDase1, 2, and 3) are expressed in the nervous system [46]. NTPDase1 and 3 hydrolyze both ATP and ADP, while NTPDase2 primarily hydrolyzes ATP with minimal ADP hydrolytic activity [47]. Extracellular AMP is further hydrolyzed to adenosine by ecto-5′-nucleotidase (CD73) [47, 48] and a transmembrane isoform of prostatic acid phosphatase (PAP) [47, 48] in the nervous system. By control of ATP degradation and adenosine generation, these ecto-nucleotidases affect nociception by terminating ATP-induced pain and pain sensitization and promoting adenosine-mediated analgesia.
ATPase activity had been detected in dorsal root ganglion (DRG) and spinal cord using enzymatic histochemistry staining. Nucleotidase activity is robust in spinal cord dorsal horn nociceptive lamina suggesting that nucleotide hydrolysis would play a role in nociceptive processing. In DRG, extensive staining revealed ecto-ATPase activity in a subset of neurons and non-neuronal cells. The mRNA expression and immunoreactivity for NTPDase1–3, but not NTPDase8, was detected in lumbar DRG and spinal cord. Immunoreactivity for NTPDase3 that closely matches the distribution of ecto-ATPase activity labels DRG central projections in the dorsal root and superficial dorsal horn, as well as intrinsic spinal neurons concentrated in lamina II. It has been reported that NTPDase3 is located in nociceptive and non-nociceptive neurons of DRG, in the dorsal horn of the spinal cord, and the free nerve endings in the skin [49]. These data suggest that NTPDase3 would be a negative regulator for nociceptive signaling [50]. However, studies from NTPDase3 knockout mouse show that deletion of NTPDase3 does not impair ATP hydrolysis in primary somatosensory neurons or dorsal spinal cord. Also, NTPDase3 (−/−) mice did not differ in nociceptive behaviors when compared with wild-type mice. These observations suggest the existence of multiple ecto-nucleotidases acting redundantly to hydrolyze nucleotides [49].
Even though the manipulation of adenosine transport or degradation can induce antinociception [51], extracellular adenosine level is mainly controlled by extracellular AMP hydrolysis. Indeed, it has been shown that extracellular AMP hydrolysis provides the major source for endogenous adenosine in the nervous system that is essential to maintain a tonic activation of adenosine receptors in the nociceptive neurons of the spinal cord [52]. Two ecto-nucleotidases have been identified to be responsible for extracellular AMP hydrolysis in the spinal cord [48]. Ecto-5′-nucleotidase (CD73) is a membrane-anchored protein that hydrolyzes extracellular adenosine 5′-monophosphate (AMP) to adenosine in different tissues. CD73 was detected in peptidergic and nonpeptidergic nociceptive neurons in DRG and afferent terminals in lamina II of spinal cord. In addition, CD73 was also located on epidermal keratinocytes, cells of the dermis, and on nociceptive terminals in the epidermis [52]. Besides CD73, prostatic acid phosphatase (PAP) also functions as an ecto-nucleotidase and generates extracellular adenosine. PAP is expressed in nociceptive dorsal root ganglia (DRG) nociceptive neurons, it had been shown that PAP inhibits noxious thermal sensitivity and sensitization that is associated with chronic pain through sustained activation of the adenosine A1 receptor [53].
Knockout of CD73 and/or PAP reduced adenosine generation and enhanced nociception in animal models following inflammation and nerve injury [52]. It has been found that AMP hydrolysis was nearly abolished in DRG neurons and lamina II of the spinal cord from PAP/CD73 double knockout (dKO) mice. Likewise, the antinociceptive effects of AMP were reduced in PAP/CD73 dKO mice. Adenosine was maximally produced from AMP within seconds in wild-type (WT) mice but was significantly reduced in dKO mice indicating PAP and CD73 generate rapidly adenosine in lamina II. Besides, it has shown the existence of spontaneous low-frequency adenosine transients in lamina II in wild-type mice, while knockout of PAP and CD73 abolished the spontaneous adenosine transit suggesting these ecto-nucleotidases rapidly hydrolyze endogenously released nucleotides to adenosine, and there exists tonic activation of A1 receptors. Field potential recordings in dorsal horn lamina II and behavioral studies indicated that adenosine converted by these enzymes acts through the A1 receptor to inhibit excitatory neurotransmission. PAP and CD73 injected spinally produced long-lasting adenosine A1 receptor-dependent antinociceptive effects in inflammatory and neuropathic pain models [54]. Furthermore, it has been noted that following peripheral nerve injury CD73, PAP, as well as enzymatic ecto-AMPase activities were reduced in dorsal horn lamina II. Collectively, these evidences indicate that PAP and CD73 are the predominate ecto-nucleotidases that generate adenosine in the nociceptive circuits (Figure 1) [48].
Schematic illustrates purinergic signaling responsible for the pain signal transmission and sensitization at the nociceptive synapses. (1) Primary nociceptive inputs promote glutamate and ATP co-release and synergistically cause non-selective permeability to Ca2+, Na+, and K+ cations via P2X3 receptor, leading to postsynaptic activation of NMDA or AMPA receptors and further contributing astrocytic glutamate and ATP co-release into the extracellular milieu which result in the pain signal transmission in the nociceptive synapses. (2) Activation of P2X4/7 receptors expressed on astrocytes and microglia induces a local inflammatory response with release of cytokines including IL-1β, BDNF, and TNF-α, which will lead to sensitization in pain signal transduction and conduction as well as synaptic transmission caused by enhanced excitatory and reduced inhibitory driving. (3) Activation of A1 receptor triggers multiple intracellular cAMP/PKA, PLC/IP3/DAG, and nitric oxide/cGMP/PKG signaling and induces analgesia by reducing both presynaptic vesicle release and postsynaptic excitability. Adenosine may also mediate antinociception by activation of A2A, A2B, or A3 receptors expressed on nociceptive neurons, astrocytes, or immune cells. (4) Ecto-nucleotidases (NTPDase3/CD73) are specifically expressed in primary nociceptive neurons and localized at presynaptic terminals that will drive the shift from ATP-induced pain to adenosine-mediated analgesia by control of extracellular ATP extracellular hydrolysis in the nociceptive pathway [99].
Dentin hypersensitivity (DHS) is defined as a short, sharp pain that arises from exposed dentin in response to various environmental stimuli [55, 56, 57]. Dentin exposure can be caused by physical, chemical, pathological, biological challenges, and/or developmental abnormalities that result in dental and or periodontal damage or defects. In patients with DHS, gentle touch, mild cold or hot, chemical (acidic or sweet fruits, foods, and drinks) or air-flow stimulation to the exposed dentine can induce similar short, sharp pain. DHS can affect the quality of patient’s daily activities such as eating, drinking, speaking, and tooth brushing. In some cases, more severe DHS can become a constant annoyance and induce psychological and emotional distractions [55, 57]. Even though DHS is a common problem, the underlying nociceptive transduction mechanism still remains elusive, and no universally accepted or highly reliable desensitizing agents or treatment are available in dental practice.
It is generally regarded that DHS is associated with dentin exposure, especially the exposure of open dentinal tubules, and dental pulp nerve responsiveness to external environmental stimuli [58]. Several theories have been proposed for the pathogenesis of DHS. The most widely accepted one is the hydrodynamic theory that is introduced by Brannstrom in 1964 [59]. It stated that environmental mechanical, thermal, or chemical changes cause the movements of fluid within dentinal tubules that stimulate the terminals of pulpal nerve fibers located at the dentin tubule inlets, thereby induces transient acute pain. The hydrodynamic theory highlights the notion that several different stimuli can evoke similar responses via dentin tubule fluid movements. The intra-dental myelinated Aβ fibers and some Aσ fibers that send terminals into the dentin tubules are thought to respond to the fluid movements resulting in the characteristic short, sharp pain of DHS. However, Aβ fibers usually mediate slight touching sensation with a lower threshold to mechanical stimulation, while Aσ fibers mediate pain, but they exhibit high threshold to noxious stimulation. How the essentially non-noxious dentin tubule fluid movements induce the nociceptive transduction in dental pulpal nerve fibers remains an enigma. Recently, the hydrodynamic theory has been challenged by emerging evidence suggesting that odontoblasts might play an essential role in the nociceptive transduction of DHS [60, 61, 62].
Odontoblasts locate at the outermost layer of the dental pulp and send odontoblastic processes to the dentin tubules. Therefore, odontoblasts are the first dental pulp cells to detect external stimuli in dentin exposure. Though a physical synaptic structure is absent, dental pulp nerve fibers are closely approached to the odontoblasts and tightly entangle these cells. This finding could provide a mechanism to explain how signals are transmitted to adjacent nerve endings through chemical mediators released from the odontoblasts. That is, a paracrine cell-cell communication is involved in signal transmission as opposed to classic neural synapses. Since purinergic P2X3 receptors are expressed in dental pulp nerve fibers [63] and activation of P2X receptors in peripheral nerve fibers induces pain [9]. ATP has been proposed as a promising candidate that participates in cell-cell communication within the dental pulp that would be associated with pain transduction mechanism of DHS [64].
For the past decades, chemo-, mechano-, and or thermo-sensitive channels such as connexin, pannexin, TRPV1-4, TRPM3, KCa, TREK-1, beta-ENa(+) C, and ASIC2 channels have been identified in odontoblasts [60, 65, 66, 67, 68, 69, 70]. Activation of these channels depolarizes the membrane potential that induces ATP release via vesicles release or channel opening in odontoblasts. Interestingly, mechanic- as well as depolarization-sensitive ATP permeable channel such as connexin 43 and pannexins had been detected in odontoblastic processes inserting into dentinal tubules [60, 64]. Indeed it has been shown that mechanical and or thermal stimulation that mimics dentin hypersensitivity in clinic induces ATP release from odontoblasts [65, 66, 71]. Besides, mechanical stimulation-induced ATP release and ATP-mediated signal transmission from odontoblasts to trigeminal neurons have been demonstrated in vitro using co-culture models comprising of odontoblasts and trigeminal neurons [68, 72]. The existence of autocrine/paracrine mechanisms for ATP-involved purinergic signaling in cultured odontoblast-like stem cells is also confirmed [73]. Furthermore, external mechanical and thermal stimulation that mimics dentin hypersensitivity induces ATP release in a tooth perfusion model, while pharmacological blocking connexin and pannexin channels abolished external stimulation-induced ATP release in dental pulp [66]. Based on the above observations, we proposed that, as illustrated in Figure 2, external stimulation-induced mechanosensitive responses and ATP release from odontoblasts and subsequently activation of purinergic receptors in dental pulpal nerves may represent a novel explanation as to how odontoblasts participate in a mechanosensory mechanism leading to the pain transduction in DHS [60, 74].
A novel hypothesis for nociception transduction in DHS. External stimulation-induced dentin tubule fluid movements induces ATP release via pannexin/connexin channels in OBs (odontoblasts), ATP then activate P2X receptors on adjacent nerve fibers to trigger the transduction of pain. ATP signaling is terminated by ecto-ATPases in OBs and Schwann’s cells.
Dentin-odontoblasts-nerve terminal complex represents the essential components for the process of stimulation transducing and nociceptive transduction from environmental changes to pain impulse in DHS. External stimuli promote ATP release from odontoblasts through mechanic or depolarization-sensitive channels, which then initiates pain signaling via activation of P2X3 receptors in dental pulp nerve fibers. Functional ecto-nucleotidases in odontoblasts, dental pulp nerve fibers, and Schwann cells that surround the nerve fibers modulate pain transmission by control of the local concentration of extracellular ATP and adenosine. ATP and its metabolites may also activate the P2Y and P1 receptors via a paracrine mechanism to trigger intracellular Ca2+ signals that further promote ATP release in odontoblasts and regulate the expression of ATP permeable channels, purinergic receptors, and ecto-nucleotidases.
The existence of mechanical-sensitive ATP permeable connexin/pannexin channels and ATP singling in dentin-odontoblast-nerve fiber complex provides a clue to explain the unique characteristic of DHS, that is, the “all” or “none” property. In patients with DHS, a common phenomenon is that external environmental stimulation induces either one sharp pain or no pain at all. A self-activated propagation of ATP signaling and calcium response in gap junction coupled cells as well as in tissues or organs was demonstrated [75]. For example, a local mechanical stimulation induces connexin/pannexin channel opening, and then result in ATP release, ATP then activates the P2X/P2Y receptors in adjacent cells inducing intracellular Ca2+ increase and/or cell depolarization that further promote connexin/pannexin channels opening and ATP release in further beyond adjacent cells until all the cells are activated. Since odontoblasts express connexin 43 and are functionally connected via gap junction as a syncytium [60, 76], stimulation from locally exposed dentin tubules will induce a response in the whole dental pulp odontoblasts. With this mechanism, external stimulation will cause the full dental pulp odontoblast activation and evoke the typical “all” or “none” short, sharp pain in patients with DHS.
The existence of ecto-ATPase activity in dental pulp nerve fibers as well as in the odontoblast layer [60] may provide mechanisms to terminate ATP-induced pain in DHS. Studies have shown that NTPDase2 is expressed in odontoblasts as well as in Schwann’s cells that encapsulate the dental pulp nerve fibers. While NTPDase3 is expressed in dental pulp nociceptive nerve fibers. The presence of these enzymes in dental pulp provides machinery responsible for ATP degradation that may provide a mechanism to terminate the pain signaling induced by purinergic receptor activation in DHS. While the existence of ecto-AMPase enzymatic activities and expression of CD73 in nociceptive nerve fibers and odontoblasts [64] will hydrolyze AMP to adenosine, the latter will activate the A1 receptors and hyperpolarize the terminals of the dental pulp nerve fibers via opening the potassium channels that will help to stop any lingering of pain impulses in nerve fibers.
Activation of P2X receptors in peripheral nociceptive nerve fibers results in pain transduction. Interestingly it has been observed that purinergic P2X receptors are preferentially expressed in trigeminal nociceptive neurons [11, 12] suggesting that purinergic signaling might play a unique role in the generation and development of dental orofacial pain. Previous studies have shown expression of P2X3 receptors in dental pulp nerve fibers, including the iB4 positive nociceptive fibers [63]. Furthermore, it had been demonstrated that activation of P2X3 and P2X2/3 receptors in dental pulp is sufficient to elicit nociceptive behavioral as well as trigeminal brainstem neuronal activity [77]. Functional homomeric P2X3 receptor and heteromeric P2X(2/3) receptor are highly expressed on nociceptive trigeminal neurons, their contribution toward the pain mechanism in dental orofacial pain has been well established [78, 79]. Using real-time reverse transcription-PCR analysis, besides P2X3, mRNA expression for P2X1 and P2X4 was also detected in trigeminal ganglion neurons. Indeed, application of P2X receptors agonists, ATP, α,β-methylene ATP, or β, γ-methylene ATP induced neuronal Ca2+ influx and a series of selective antagonists for P2X1, P2X3, or P2X4 receptors inhibited these Ca2+ influx responses. Interestingly, expression of purinergic receptors (P2X1, 3, and 5) in trigeminal ganglion is upregulated in response to dental pulp inflammation-induced pain suggesting that these receptors may participate in the peripheral pain sensitization [80]. Expression of P2X receptors in trigeminal ganglion is also upregulated by oral facial deep tissue inflammation [11, 12]. In addition, application of P2X receptor agonist αβ-meATP to rat tooth pulp induces central sensitization in medullary nociceptive neurons, and this sensitization response can be blocked by dental pulp application of the P2X (1,2/3,3) receptor antagonist TNP-ATP as well as by medullary application of TNP-ATP. These results suggest that the activation of peripheral P2X receptors in orofacial tissues plays a critical role in producing central sensitization in medullary trigeminal subnucleus caudalis (TSNC) nociceptive neurons [81]. Therefore, trigeminal ganglion neurons preferentially express functional P2X1, 2/3, 4 receptors, and activation of these receptors attributes to generation and sensitization of dental orofacial pain [78].
Involvement of P2X receptor activation in dental orofacial pain had been demonstrated in various animal models. In the carrageenan-induced TMJ inflammatory hyperalgesia model, the P2X1, 3, and 2/3 receptor antagonist TNP-ATP, but not the selective P2X7 receptor antagonist A-438079, significantly reduced the pain behavior. These findings indicate that P2X3 and P2X2/3 receptors would be potential targets for the development of new analgesics to control TMJ inflammatory pain [82]. Interestingly, it has been found that the number of P2X3 receptor positive cells is increased in the small cell group in trigeminal ganglia, whereas there was no change in medium or large cell groups after TMJ CFA-injection. Retrograde tracing confirmed that TMJ-innervated neurons in TG exhibited P2X3 receptors. These observations provided evidence to support that P2X3 receptor play an essential role in orofacial pain induced by TMJ arthritis [83]. Pharmacological and immunohistochemical studies revealed that the P2X3 receptor also plays an essential role in the heat hyperalgesia observed in the infraorbital nerve (IoN) ligation-induced neuropathic pain model [84]. In an oral cancer pain model, injection of squamous cell carcinoma cells into the lower gingiva produces mechanical allodynia and thermal hyperalgesia. It has been observed that expression of P2X receptor, calcitonin gene-related peptide (CGRP)-, substance P (SP)-, and capsaicin receptor (TRPV1)-immunoreactive cells are strikingly upregulated in the small cell group of trigeminal ganglia (TGs) after tumor cell inoculation [85].
Whereas there is ample evidence that purinergic P2 receptors in trigeminal glial cells are altered after peripheral nerve injury, there is very little information about the changes of P2 receptors in TG satellite glial cells (SGCs), although it is well established that SGCs are endowed with P2 receptors. In submandibular inflammation with the injection of complete Freund\'s adjuvant, there was a marked increase in the sensitivity of SGCs to ATP, with a threshold decreasing from 5 μM to 10 nM. A similar result was observed in the intact trigeminal ganglion after infraorbital nerve axotomy. It had been demonstrated that the increased after-inflammation response was mediated predominantly by P2X receptors. The enhanced responses to ATP after inflammation are primarily due to P2X2 and or P2X5 receptors, with a possible contribution of P2X4 receptors. It has been proposed that the over 100-fold augmented sensitivity of SGCs to ATP may contribute to the development of chronic pain status in dental orofacial pain [86].
Little is known about P2Y receptor expression in trigeminal nerves and their role in dental orofacial pain. It had been demonstrated that UTP, an agonist of P2Y2/P2Y4 receptors, significantly decreased the mean threshold potentials for evoking action potentials and induced a striking increase in the mean number of spikes in TG neurons [87]. Because of its vital role in the control of neuronal spike onset, fast inactivating transient K+ channels (IA) is a key regulator of membrane excitability in sensory neurons. It has been shown that UTP significantly inhibited IA and the expression of Kv1.4, Kv3.4, and Kv4.2 subunits in TG neurons. The P2Y receptor antagonist suramin could reverse these effects. Furthermore, in ION-CCI (chronic constriction injury of the infraorbital nerve) induced neuropathic pain model, when blocking P2Y2 receptors with suramin or injection of P2Y2 receptor antisense oligodeoxynucleotides led to a long time- and dose-dependent reverse of allodynia [87]. Blocking P2Y2 receptors is accompanied with a significant increase in Kv1.4, Kv3.4, and Kv4.2 subunit expression and decrease in phosphorylated ERK expression in trigeminal ganglia. These data suggest activation of P2Y2 receptors leads to upregulation of ERK-mediated phosphorylation and decline of the expression of I(A)-related Kv channels in trigeminal ganglion neurons, which might reveal potential alternative targets for the treatment of trigeminal neuropathic pain [87].
Other type of P2Y receptors are also involved in the development of dental orofacial pain. Administration of the P2Y1, 12, and 13 receptor agonist, 2-(methylthio)adenosine 5′-diphosphate trisodium salt hydrate (2-MeSADP), in naïve rats induced neuropathic pain in the tongue, as demonstrated in lingual nerve crush rats, while co-administration of P2Y receptor antagonists (MRS2395) to naïve MRS2395 rats did not result in hypersensitivity of the tongue. P2Y12 receptor had been detected in satellite cells of the trigeminal ganglia. In an orofacial pain model after lingual nerve crush, expression of P2Y12 receptors was enhanced in pERK1/2-immunoreactive cells encircling trigeminal ganglion neurons. Administration of a selective P2Y12 receptor antagonist, MRS2395, attenuated tongue hypersensitivity to mechanical and heat stimulation and suppressed the increase in the relative numbers of calcitonin gene-related peptide (CGRP)-immunoreactive neurons and neurons encircled by pERK1/2-immunoreactive cells. These results suggest that intercellular communication between activated satellite cells and CGRP-immunoreactive neurons via P2Y12 receptors contributes to the development of orofacial neuropathic pain [88].
Besides purinergic receptors expressed in the central afferent terminals of primary trigeminal nociceptive neurons, multiple P2X, P2Y, and P1 receptors are also detected in the secondary nociceptive neurons, astrocytes, and microglia in TSNC. Since pain signal synaptic transmission is accompanied by a large amount of ATP release in TSNC. Activation of purinergic receptors expressed in presynaptic afferent terminals, secondary nociceptive neurons, astrocytes, and microglia in TSNC would play an essential role for the development of central sensitization [77]. Studies have shown that extracellular ATP acting on presynaptic purinergic receptors (P2X2/3 and P2X3 subunits) participate in central sensitization of dental orofacial pain. Application of inflammatory irritant mustard oil (MO) to the tooth pulp produced a long-lasting allodynia and hyperalgesia. Intrathecal administration of the selective P2X1, P2X3, and P2X2/3 receptor antagonist, TNP-ATP, significantly and reversibly attenuated the MO-induced central sensitization. While the administration of the selective P2X1, P2X3, and P2X2/3 receptor agonist, alpha, beta-methylene ATP (alpha, beta-meATP, i.t.) produced abrupt and significant neuroplastic changes in TSNC nociceptive neurons, followed by neuronal sensitization as evidenced by the ineffectiveness of a second application of alpha, beta-meATP and subsequent MO application to the pulp. These results suggest that P2X3 and possibly also the P2X2/3 receptor subtypes in TSNC play a crucial role for the initiation and maintenance of central sensitization in brainstem nociceptive neurons [89]. Tooth pulp application of mustard oil (MO) induced a significant increase in glutamate release in TSNC. Intrathecal administration of apyrase or TNP-ATP (a P2X1, P2X3, P2X2/3 receptor antagonist) alone significantly reduced the MO-induced glutamate release in the TSNC. Furthermore, the suppressive effects of apyrase on glutamate release were reduced by DPCPX (an adenosine A1 receptor antagonist) [89].
It had been reported that P2X3 receptor expressed in astrocytes in the TSNC participates in the development of craniofacial neuropathic pain induced by chronic constriction of the infraorbital nerve (CCI-ION) [90]. The number of P2X3-positive fine astrocytic processes and the density of P2X3 receptors in these processes was increased significantly in CCI-ION model and administration of MPEP, a specific mGluR5 antagonist, alleviated the mechanical allodynia and abolished the increase of P2X3 receptor expression in the fine astrocytic processes. Specific glial cell populations become activated in both trigeminal ganglia and brainstem in CFA-injection induced temporomandibular joint (TMJ) inflammation pain model. CFA-injected animals exhibited ipsilateral mechanical allodynia that is accompanied by a substantial increase of GFAP-positive satellite glial cells and activation of resident macrophages in the trigeminal ganglia. The activated microglial cells were also observed in the ipsilateral TSNC [91]. In dental pulp, MO injection induced central sensitization model, it has been demonstrated that continuous intrathecal (i.t.) superfusion of the potent P2X7 receptor antagonists brilliant blue G or periodate-oxidized ATP could significantly attenuate the central sensitization. Specifically, central sensitization could be induced by superfusion of ATP and even more effectively produced by the P2X7 receptor agonist benzoylbenzoyl ATP. Consistent with the report that P2X7 receptors are mostly expressed on microglia, superfusion of the microglial blocker minocycline abolished the MO-induced central sensitization. These novel findings suggest that activation of P2X7 receptors in microglia cells may be involved in the development of central sensitization in acute dental orofacial pain [92].
Microglial P2Y12 receptor is also reported to be involved in the central sensitization of orofacial pain [93]. In a tongue cancer, pain model produced by squamous cell carcinoma (SCC) cell inoculation, microglia were strongly activated in TSNC, and administration of MRS2395 or minocycline reversed the associated nociceptive behavior and microglial activation in SCC-inoculated rats. The increased activity of TSNC wide dynamic range nociceptive neurons was also recorded in SCC-inoculated rats. These findings suggest that SCC inoculation results in strong activation of microglia via P2Y12 receptor signaling in the TSNC that is associated with the increased excitability of TSNC nociceptive neurons and the development of central sensitization.
Purinergic P1 receptor signaling may also exist in trigeminal nerves and affects nociception processing. In 12 healthy female volunteers randomized, double-blind, placebo-controlled, cross-over trial, the effect of A1 receptor agonist GR79236 on trigeminal nociception processing was investigated. Activation of A1 receptor with GR79236 inhibits trigeminal nociception in humans [94]. In a model of trigeminovascular nociceptive transmission, the superior sagittal sinus (SSS) was stimulated electrically, and the responding nociceptive units were recorded. It has been shown that intravenous administration of the highly selective adenosine A1 receptor agonist, GR79236 had a dose-dependent inhibitory effect on SSS-evoked trigeminal nociceptive activity. Selective adenosine A1 receptor antagonist DPCPX abolished the neuronal inhibitory effect of GR79236 [95]. In another animal experiment, adenosine decreased the amplitude of glutamatergic excitatory postsynaptic currents and increased the unpaired-pulse ratio suggesting that adenosine acts presynaptically to reduce glutamate release from primary afferents. Besides, the adenosine-induced inhibition of excitatory postsynaptic currents was impaired by a selective A1 receptor antagonist, DPCPX, and was mimicked by a selective A1 receptor agonist CPA. These findings suggest that presynaptic A1 receptors decrease action potential-dependent glutamate release from primary trigeminal afferents onto TSNC neurons, and thus adenosine A1 receptors could be a potential target for the treatment of pain of orofacial tissues [96].
By the control of ATP degradation and adenosine generation, ecto-nucleotidases drive the shift from ATP-induced nociception to adenosine-induced analgesia [97]. Since ATP induces pain and pain sensitization via activation of P2X receptors and adenosine mediates analgesia via activation of P1 receptors, existence of ecto-nucleotidases and their enzymatic activities in the trigeminal nociceptive pathway will affect the development and maintenance of dental orofacial pain. Recently we have demonstrated the expression and central terminal localization of ecto-nucleotidases (NTPDase3/CD73) in the trigeminal ganglia nociceptive neurons [64, 98]. Considering the pivotal role of purinergic singling in the pathogenesis of neuropathic pain and the preference expression and upregulation of purinergic receptors in the trigeminal nervous system, ecto-nucleotidase expression, and localization in trigeminal nerves might participate in the development of orofacial neuropathic pain.
Using histochemistry staining, ecto-ATPase and AMPase activities were detected in dental pulp odontoblast layer, Raschkow’s nerve plexus, and nerve bundles. Interestingly, in inflammatory dental pulp with pulpitis, enzymatic ecto-ATPase activity was significantly upregulated. Specifically, using immunohistochemistry and immunofluorescence staining, NTPDase2 is expressed in Shwann’s cells that encapsulate the Aβ and Aσ fibers, while that NTPDase3 and CD73 are detected in nociceptive nerve fibers in dental pulp [60, 64, 98].
Trigeminal ganglia contain both primary sensory neurons and satellite glial cells. Satellite glial cells encapsulate the ganglia neurons and are gap junction channel connected. Via intercellular interaction satellite glia cells affect neuronal excitability and impulse conduction in TG neurons. The ecto-ATPase activity was detected in TG cells. Specifically, NTPDase3 is expressed in TG neurons, including the nociceptive neurons, while NTPDase2 is expressed in TG satellite glial cells that encapsulated the TG neurons [60, 64, 98]. In addition, ecto-AMPases activity is also detected in TG cells and TG nerve fibers. It reveals that CD73 is expressed in TG neurons, including the nociceptive neurons [64]. By control of extracellular ATP degradation and adenosine generation, these enzymes would play a crucial role in orofacial pain signal processing by affecting the excitability, inhibition, and interaction of TG neurons.
TG nociceptive neurons project central nerve fibers to the brainstem and form synapses with the secondary nociceptive neurons in the nociceptive lamina of the TSNC. It has been well established that the nociceptive lamina in the brainstem or spinal cord is a pivotal region for pain signaling transmission, inhibition, modulation, and sensitization. Interestingly, striking ecto-ATPase and ecto-AMPase activities were detected in brainstem TSNC nociceptive lamina. Immunohistochemistry studies confirmed the existence of immunoreactivity for NTPDase3 and CD73 in the nociceptive lamina. Furthermore, it has been demonstrated that incubation with specific anti-NTPDase3 or anti-CD73 antibodies, significantly reduced ecto-ATPase and acto-AMPase activities in TNSC nociceptive lamina, respectively [64, 98]. These findings suggest that NTPDase 3 and CD73 are the major enzymes responsible for ATP degradation and adenosine generation in TSNC nociceptive lamina. Since the neuronal plasticity and central sensitization mainly occurs at the central nociceptive lamina in neuropathic pain, the presence of NTPDase3 and CD73 in TNSC nociceptive lamina may also participate in the central sensitization mechanism in orofacial neuropathic pain.
The characteristic staining patterns for NTPDase3 and CD73 in the nociceptive lamia of TSNC indicate the presynaptic localization of these enzymes [64, 98]. This observation suggests that NTPDase3 and CD73 are produced at TG nociceptive neurons and then are transferred to the central presynaptic membranes along the afferent trigeminal nerves. Disruption of ecto-nucleotidase expression and presynaptic localization caused by biological, chemical, or physical trigeminal insults such as virus infection, nerve fiber differentiation, and physical constriction//compression may attribute to pathogenesis mechanism in trigeminal neuralgia and other orofacial neuropathic pain [64, 98].
Purinergic signaling plays essential role in pain signal processing in the nociceptive pathway from peripheral to central nerves. Via activation of P2X, P2Y, and P1 receptors, ATP and its metabolites induced purinergic signaling participates in the nociceptive transduction, conduction, transmission, modulation, sensitization, and development of neuropathic pain. Ecto-nucleotidases are the predominant enzymes responsible for extracellular ATP degradation and adenosine generation that play essential role to drive the shift from ATP-induced pain to adenosine-induced analgesia. In order to identify the role of purinergic signaling in dental orofacial pain, the existence of purinergic signaling and their regulation in the trigeminal nociceptive pathway has yet to be identified.
Several ion channels and receptors that are prominent in craniofacial nociceptive mechanisms have been identified on trigeminal primary afferent neurons. Many of these receptors and channels exhibit unusual distributions compared with extracranial regions. For example, expression of the ATP receptor P2X3 is strongly implicated in nociception and is more abundant on trigeminal primary afferent neurons than analogous extracranial neurons. P2X3 receptors are often co-expressed with the nociceptive neuropeptides CGRP and SP in trigeminal ganglia neurons. Co-expression of P2X3 receptor and other nociceptors (TRPV1, and ASIC3) in trigeminal neurons imply the existence of functional complexes that allow craniofacial nociceptive neurons to respond synergistically to altered ATP and other pain mediators. These observations indicate that trigeminal P2X3 receptor expression pattern differs markedly from dorsal root ganglion that may provide a clue to explain the unique properties of dental orofacial pain. Different expression and or regulation of purinergic signaling in the trigeminal nociceptive pathway may attribute to a nociceptive mechanism of dentin hypersensitivity and dental orofacial pain. Identification of the underlying nociceptive mechanism will unveil potential targets for better treatment and management of dental orofacial pain.
Internal geodynamics is manifested on the Earth’s surface by volcanic phenomena. Most of these phenomena are controlled by volcanoes located in the tectonically and structurally weak areas of the globe, notably accretion zones, convergence zones, and intra-plate zones. Some of these volcanoes are characterized by a simple crater, while others have one or more complex craters (distinguished by the collapse events). These complex craters are defined by one or more calderas [1, 2, 3, 4]. The term caldera derives from the depression called Taburiente (Canary Islands) and has been firstly used by [5]. The Caldera de Taburiente in fact, is the frequently quoted example of erosion caldera. Erosion calderas are volcanic depression erosionally formed on the summit or on the flanks of the volcano, which may be several kilometers in diameter [6, 7, 8]. However, geologically, calderas are volcanic depressions resulting from the collapse of the roof of the magma chamber due to the rapid retreat of the magma during an eruption [9, 10]. They can be elliptical, sub-circular or circular in map view. These shapes are induced by the shape of the underlying magma reservoir [11, 12]. In Refs. [9, 13], five types of collapse such as piston, piecemeal, trapdoor, downsag, and funnel have been defined to ease the comprehension of the caldera formation processes.
\nNevertheless, insufficient work on the dynamics of caldera emplacement limits the understanding of the functioning and evolution of volcanic massifs worldwide. Some calderas deserve to be characterized according to the models of [9] and [13] in order to classify them according to the Collapse Caldera DataBase established by [14]. The Collapse Caldera DataBase makes it possible to better study the caldera formation processes and to classify them. The study of calderas for decades has been of paramount importance for the development of science; it allows us to understand the functioning of volcanic apparatus around the world and the environmental impact that can result from them. Since calderas constitute a natural heritage for the economic development of several countries and a laboratory for education and research [15, 16, 17], their classification will heighten their promotion and valorization.
\nMount Bambouto, which was once a very active volcano, was truncated at their summit by a caldera like some volcanoes along the Cameroon Volcanic Line (Figure 1). It caldera was chosen for the present study because Mount Bambouto have been the subject of numerous studies focusing mainly on petrography, geochemistry, geochronology, geo-heritage, hazards and associated risks [18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28, 29]. With the exception of [20, 21, 29], the studies on the caldera of Mount Bambouto are generally carried out in the specific areas [22, 30, 31]. Mount Bambouto is the third largest volcano (in volume) in the Cameroon Volcanic Line after Mount Cameroon and Mount Manengouba. It is located in the NE extension of Mount Manengouba from which it is separated by the Mbô plain. It is almost continuously contiguous to the NE with Mount Bamenda and covers an area of about 800 km2. It is located between longitudes 09°55′ and 10°15′E and latitudes 05°25′ and 05°50′N. They straddle the Departments of Bamboutos in the East, Menoua in the South, Lebialem in the West and Mezam in the NW and, culminate at 2744 m at Meletan Mountain where they dominate the West Cameroon Highlands. Mount Bambouto is a huge shield volcano with a general SW-NE orientation [18]. This massif is characterized by the asymmetry of its slopes [32]. Its summit caldera is located between longitudes 09°57′ and 10°07′E and latitudes 05°37′ and 05°44′N. The Caldera of the Mount Bambouto has an elliptical map view (16 × 8 km) that opens in a horseshoe shape toward the west (Figure 2). Throughout the caldera, rocks (basalts, hawaiites, mugearites, phonolites, trachytes, and ignimbrites) are found in different forms: flows, domes, peaks, teeth and needles that characterize the interior, the external slopes and the floor of the caldera. Thus, the inside of the caldera is marked by a sinuous “s” line punctuated by trachytic and phonolitic peaks, necks, and domes [18, 20, 29]. Moreover, the crystalline basement made up of granite, is observed on the western side of the volcano [21, 22, 29]. The floor of the caldera has a structure of stairs decreasing from the east to the west of the massif. The caldera rims are sub-vertical to vertical. In addition, several steep valleys (in “v” shape) accidentally affect the topography of the whole caldera (about 78% of the slopes are susceptible to mass movements) [29].
\nThe Cameroon volcanic line.
Satellite image of the Mount Bambouto caldera.
Despite these previous studies, the dynamics of the establishment of the caldera of the Mount Bambouto remains poorly understood. Moreover, that caldera is not yet classified in the Caldera DataBase established by [10]. However, some data do exist on this caldera. These data need to be completed and this will allow us to characterize that caldera according to the model of [9]. This characterization will make it possible to obtain and organize the data in order to classify the caldera of the Mount Bambouto in the Caldera Database of [14]. This work is essential for understanding the functioning and evolution of the Mount Bambouto and, consequently, the dynamics of the Cameroon Volcanic Line, which remains a subject of discussion by many researchers nowadays.
\nSeveral field trips were made. They made it possible to describe rock outcrops, take rock samples and take the coordinates of the various samples. These samples were then described and labeled. In the laboratory, the coordinates of the various rock sampling points were plotted on the topographic map of the study area. Through these different points and the macroscopic description of the samples, a geological map is produced [33]. In order to complete the macroscopic study of the rocks, thin sections of samples were taken at the University of Orleans and the University of Paris-Sud (Orsay Campus) in France. These thin sections were studied with the polarizing microscope of the Laboratory of Environmental Geology of the University of Dschang and at the Laboratory of Life and Earth Sciences of the University of Maroua. Some samples were analyzed with microprobe also at the University of Orleans and the University Paris-Sud (Orsay Campus) and in Nancy for the nomenclature of rock minerals and the determination of the nature of rocks. These microscopic and chemical studies have made it possible to refine the geological map of the caldera of the Mount Bambouto [33]. In addition, some complementary geochemical analyses were made to determine the chemical nature of different lavas.
\nFor the volcanological evolution of the caldera of the Mount Bambouto we have:
carried out a cartographic study through the analysis of satellite images, about 70 aerial photos, digital elevation models, and topographic maps. This study allowed us to determine the exact boundaries and structure of the caldera.
The geochronological data available in the literature made it possible to produce through DTM, the different stages of caldera formation according to the model of [9].
For the classification of the Caldera of the Mount Bambouto, we used the Caldera DataBase from [14]. To do so, we used the data obtained through volcanological studies and those existing in the literature.
\nIn the Caldera of the Mount Bambouto the flows, mostly trachytic, have extensions ranging from 150 to 250 m; with an average height of between 10 and 30 m. They are generally roughly and irregularly priced and are observable at the level of the caldera ramparts, on certain escarpments, road embankments and riverbeds. On the other hand, mafic lava flows are poorly represented in the caldera and have extensions of just a few meters. The domes are generally circular to sub-circular in shape with a base slightly above the top. They are dominated by coarse prisms and sometimes numerous diaclases which favor the sporadic detachment of polygonal blocks generally observable at their base. Felsic and mafic flows are also observable in polygonal blocks accumulated near caldera ramparts and on stream beds (Figure 3). The lava texture is mostly microlitic porphyritic except for ignimbrites, which have a vitroclastic texture.
\nSome geological features of the Mount Bambouto caldera: (A–C)—post-caldera protrusions. (D)—erratic boulders; (E–G)—caldera’s floor structure; and (H)—caldera rim.
Basalts, hawaiites and trachytes all have a grayish alteration patina and are less than 3 mm thick. However, this patina has, in some places, crystals of automorphic alkaline feldspar of 4 mm or less in size. Ignimbrites have a strong patina of less than 3 mm thick and are gray to brown.
\n\nBasalts (Figures 4 and 5) are characterized by a porphyritic microlitic texture in which pyroxene phenocrystals (10–25% of the rock), plagioclase (1–3% of the rock), olivine (2–7% of the rock) and opaque oxides (<3% of the rock) are embedded in a microlitic mesostase.
\nDrawings of some thin sections of rocks in the Mount Bambouto caldera: (A)—basalts; (B)—phonolites; (C)—kaersutite-mugearite; and (D)—ignimbrites.
Photographs of thin sections of rocks in the Mount Bambouto caldera: (A, D, and H)—hawaiites; (B)—phonolites; (C, F, and G)—Basalts; (E)—trachytes.
\nHawaiites (Figure 4) are also characterized by a porphyritic microlitic texture in which pyroxene phenocrystals (2–5% of the rock), plagioclase (3–10% of the rock), olivine (15–35% of the rock) and opaque oxides (5–7% of the rock) are embedded in a microlitic mesostase.
\n\nMugearites (Figure 5) are dominated by a subporphyritic microlitic texture materialized by amphibole (kaersutite), apatite and oxide phenocrystals. These phenocrystals constitute less than 10% of the rock. These rocks are kaersutite mugaearites.
\nGenerally speaking, the trachytes (Figure 4) of the Mount Bambouto Caldera have a subporphyritic microlitic texture rich in phenocrystals of alkaline feldspar (30% of the rock), plagioclase, pyroxene (<4% of the rock), amphibole (<1% of the rock), oxide (5% of the rock) and apatite.
\n\nPhonolites (Figures 4 and 5) show a light brown alteration patina of almost 3 mm thick. The fresh, greenish gray to greenish gray sample shows large crystals of alkaline feldspar (30% of the rock); 0.5 to 5 mm in size and some pyroxene granules. Microscopically, the rock has a subaphyric to porphyritic microlitic texture containing phenocrystals and microcrystals of alkali feldspars, pyroxene, feldspathoid, amphiboles and oxides.
\n\nIgnimbrites (Figures 4 and 5) have a vitroclastic texture dominated by a facies-dominated matrix and whole or broken sections of alkali feldspar, quartz, pyroxene, and rock enclaves (trachytes and basement) in the form of rounded balls or subangular fragments.
\nIn the caldera of the Mount Bambouto, olivine is present in the basalts with an average size of 0.5 × 3 mm. It is automorphic to subautomorphic. Their section is traversed by numerous cracks along which one notes the beginning of iddingsitization and serpentinization. Some sections have a core and borders corroded by mesostase. The olivine in the caldera of the Mount Bambouto is globally magnesian with forsterite contents between Fo57 and Fo75 (Figure 6).
\nEvolution of the forsterite content in lavas in the Mount Bambouto caldera.
The lava oxides in the study area are represented by titanomagnetite and ilmenite (Figure 7). These two minerals coexist in some lava, notably dolerite mugaearites. They are sometimes automorphic with various shapes (square, rectangular and rod-shaped), with sizes ranging from 0.2 to 1 mm. They occur as phenocrystals and microcrystals either embedded in minerals such as olivine, clinopyroxene and feldspars; or embedded in mesostase. Furthermore, titanomagnetite appears as the most abundant oxide in basalts, mugaearites and trachyes.
\nPosition of oxides of lavas of the Mount Bambouto caldera in the FeO-TiO2-Fe2O3 diagram.
Apatite is observed in almost all the lavas of the caldera of the Mount Bambouto. It occurs as elongated crystals, xenomorphic to sub-automorphic and sometimes with transverse breaks in the intermediate lavas. Their size is between 0.2 and 0.8 mm and is observable as inclusions in olivine, oxides, and alkaline feldspars.
\nIn the caldera of Mount Bambouto, clinopyroxenes in lavas are found in most sub-automorphic to automorphic crystal rocks with an average size of 0.5 × 1 mm. They show two directions of cleavage in some sections. They show gulfs of corrosion in some sections. They are cracked in the trachytes and show a macle h1 in the basalts. The classification of [34] has made it possible to identify three types of clinopyroxene in the lavas of the caldera of Mount Bambouto (Figure 8); diopside, augite and hedenbergite.
\nClassification of clinopyroxènes of lavas of the mount Bambouto caldera in the en-Wo-Fs diagram.
Feldspars are the minerals most represented in the lava of the caldera of the Mount Bambouto. Their edges are corroded in certain sections of the phonolites. However, they are sub-automorphic to automorphic, cracked and elongated depending on the flow. They are found in microlites and phenocrystals with sizes ranging from 0.1 × 0.3 to 0.5 × 0.8 mm for plagioclases and from 0.1 × 0.4 to 1 × 2 mm for alkaline feldspars. The latter have a Carlsbad twin, unlike plagioclases with a polysynthetic twin. The most frequent plagioclases (An30-60) in lava are andesine and labrador. In phonolites, the alkaline feldspars are anorthose (Or17 and Or37) and sanidine (Or37 and Or44) (Figure 9). However, anorthoses are in the majority. In ignimbrites, the composition of alkali feldspars is between Or33 and Or37 and are therefore exclusively anorthoses.
\nEvolution of the anorthite content in lavas of the Mount Bambouto caldera.
The lavas in the caldera of Mount Bambouto are alkaline in nature as shown in the following diagrams in Figure 10. The data used to make these diagrams have been supplemented by the data in [20, 22].
\nChemical nature of lavas in the Mount Bambouto caldera.
Mount Bambouto is a Hawaiian shield volcano [18]. Its history has been ruled by volcanic and tectonic events that led to the formation of a huge caldera on the Pan-African granitoid basement [35, 36, 37]. The Mount Bambouto Caldera formation (Figure 11) included three main stages [38] as follow:
The Precaldera Stage (Over 19 Ma) is characterized by the tumescence of the volcanic shield due to magma injection giving rise to several annular fissures observed in the whole volcano.
The Syncaldera stage (18–15.28 Ma) is materialized by two features: firstly, explosive eruptions are responsible for scoria, ignimbrites, trachytes and rhyolites; secondly, piecemeal intravolcanic collapse of the magmatic chamber roof is followed by the protrusion of trachytic domes and some basaltic supplies.
The Postcaldera stage (15–0.5 Ma) is typified by some trachytic and basaltic supplies and the protrusion of phonolitic domes. Activity ends with the explosive eruptions on the northeastern flank of the volcano where is built the multiple scoria cones.
Sketch highlighting the stages of the formation of the Mount Bambouto caldera.
To assign the code of a given caldera, one must use the numbering system developed in the Catalog of Active Volcanoes of the World. In fact, the world is divided in 19 main regions that are subdivided, in turn, in several subregions. Hence, the study area is located in the African Region with the corresponding database code 2. In addition, these calderas are located in the Central African Sub-Region with the corresponding database code 203.
\nIn the caldera ramparts are almost vertical at some levels (Figure 3); but on the whole these ramparts seem to merge with the floor.
\nAt the level of the Mount Bambouto, the floor of the caldera is very dissected and presents in places a stepped structure (Figure 3), which indicates a piecemeal collapse.
\nSeveral petrographic types are observed in the study area. These petrographic types are dominated by basalts, intermediate rocks, trachytes, phonolites and ignimbrites. Thus, the caldera of the Mount Bambouto is assigned the code B, I, T, P and Ig.
\nThe study area is characterized by an alkaline magmatic series as they are dominated by mafic, intermediate, and felsic terms. They are assigned the codes ALKAf (Alkaline felsic), ALKAi (Alkaline intermediate) and ALKAm (Alkaline mafic).
\nMount Bambouto rests on a granito-gneissic bedrock with a thickness (hc) of about 35.5 km [39]. According to the Database [14], these crustal thicknesses in the study areas are greater than the 30–35 km interval; hence the code is C.
\nFrom the internal geodynamic point of view, the Mount Bambouto Caldera is located in the Cameroon Volcanic Line which originates, according to some authors [40, 41, 42, 43], from a Continental Rift; Its code is be RC. This nascent rift [44, 45], at the origin of the Cameroon Volcanic Line in general and of Mount Bambouto and its respective caldera system in particular, is of the extensional type and their code is EXT.
\nA Pre-caldera regional dome occurred through a tumescence that created numerous concentric faults. These fissures favored a pre-caldera magmatic activity that further contributed to the building of the Bambouto stratovolcano. Its code is therefore STR.
\nThe collapse of the Caldera of Mount Bambouto occurred at the beginning of the sequence of eruptions that contributed to their formation. Their code is A.
\nIn the Mount Bambouto, this volcanic activity is dominated by the presence of several eruptive vents, notably on the ramparts, the eastern floor of the caldera and the NE slope of the volcano. Thus, the Mount Bambouto is classified as Type-S and Type-MS.
\nOn the other hand, the ramparts of the Mount Bambouto Caldera are threatened by growing urbanization and agro-pastoral activity, particularly to the south and east of the caldera. Its boundaries are therefore slightly destroyed. Its code is PD.
\nThe overall results have been used to fill the CCDB table (Table 1).
\nCollapse caldera database | \nCriteria | \nData | \n
Latitude | \n05°37′–05°44′N | \n|
Longitude | \n09°57′–10°07′E | \n|
Region | \n2 | \n|
Subregion | \n203 | \n|
Age (Ma) | \n15 | \n|
Maximum Caldera diameter | \nNot Applicable | \n|
Minimum Caldera diameter | \nNot Applicable | \n|
Surface (km2) | \n155.1 | \n|
Subsidence | \n— | \n|
Caldera volume (km3) | \n— | \n|
Type of collapse | \nPiecemeal | \n|
Name linked to the deposits | \nIgnimbritic | \n|
Thickness of deposits | \n— | \n|
Volume of deposits (km3) | \n— | \n|
Total volume of lavas (km3) | \n— | \n|
Petrographic types | \nB, I, T, P | \n|
Magmatic series | \nALKAm, ALKAi, ALKAf | \n|
Magmatic chamber depth (km) | \n35.5 | \n|
Ratio depth/width of magmatic chamber | \n— | \n|
Plate tectonic setting (PTS) | \nRC | \n|
Crustal type (CT) | \nC | \n|
Type of tectonic faulting (TF) | \nExt | \n|
Periods of pre-caldera doming (PCD) | \nOver 19 Ma | \n|
Type of pre-caldera volcanism (PCV) | \nSTR | \n|
Timing of caldera onset (TCO) | \nA | \n|
Post-caldera volcanic activity (PCVA) | \nS, MS | \n|
Post-caldera resurgence (PCR) | \nAbsence | \n|
Caldera preservation (CPR) | \nPD | \n
Classification of the Mount Bambouto caldera in the CCDB of [10].
Through the mode of outcropping of different rocks in the caldera of Mount Bambouto, all types of dynamism (extrusive, effusive, explosive) exist in the caldera. These are therefore polygenic volcanoes marked by long periods of activity and varied dynamisms, resting and erosion phases during different tectonic episodes [46]. In addition, the diversity of rocks is indicative of the high degree of magma differentiation induced here by the fractional crystallization process [21, 47, 48]. The presence of the trachytes in ignimbrites of the study area is an indicator of a relative chronology of the rocks. Indeed, there was an ante-ignimbritic trachytic volcanic phase. This means that there has been in the course of the evolution of the Bambouto volcano, the eruption of trachytic rocks before that of ignimbritic materials [49, 50].
\nThe caldera of Mount Bambouto was formed at a well-defined time. The stages of formation of these calderas correspond globally to the model of [9]: a regional tumescence, a volcanic eruption, a collapse of the caldera, volcanism on the annular fractures and sedimentation. The present structure of the caldera floor shows that the roof of the magma chamber collapsed piecemeal during its formation. The border faults generally observed on calderas in certain volcanic environments in Cameroon, which are evidence of the different phases of caldera collapse, are difficult to observe in the caldera of Mount Bambouto. These faults, when identifiable on certain ramparts, present a some stages of collapse (Figure 3). In this caldera, the ramparts are often confused with the floor. The latter constitutes the most dissected floor of all the caldera units studied along the Cameroon Volcanic Line and their arrangement in decreasing steps from west to east, would testify to the multiple collapses that marked its formation [51, 52]. On the other hand, in the Eboga and Lefo calderas, where the ramparts are clearly visible from the caldera floor, there are boundary faults marked by about 2–4 stages of collapse [29]. Post-caldera volcanism has manifested itself on the Mount Bambouto. This has been observed in other caldera environments on the Cameroon Volcanic Line, notably the Santa-Mbu and Lefo caldera in the Bamenda Mountains, the Eboga and Elengoum calderas in Mount Manengouba and the Bangou caldera in Mount Bangou. It is at the origin of numerous doleritic, phonolitic and trachytic protrusions and, cones and maars found on the floor and external slopes of these calderas [33, 51, 52, 53, 54]. These post-caldera geomorphological units give the caldera of Mount Bambouto the S and MS types according to [14]. Mount Bambouto constitutes a stratovolcano [20, 33]. The shape of this caldera is comparable to the elliptical shape of the calderas of Suswa, Kenya [55] and Chã das of Fogo Island in Cape Verde [56] and the calderas of the basaltic shields described by [9, 57]. This shape results from the geometry of the magma chamber which is the main factor controlling the final morphology of the calderas [58]. The presence of ignimbrites, tuffs, trachytes and rhyolites in the caldera of the Mount Bambouto qualifies it as an ignimbrite caldera. Ignimbrite calderas are usually over 10 km in diameter and over 1 km in depth, formed after the voluminous deposition of silicic ignimbrites [9, 11, 59]. We can list the example of Batur Caldera in Bali, New Zealand [60]. However, the term ignimbrite caldera is clearly used by (2015) [61] to qualify the calderas of the Southern Rocky Mountain Volcanic Field in Colorado (USA) notably Bonanza, Bachelor, Cochetopa Park, Creede, and Platoro calderas. Their presence in Mount Bambouto is explained by the fact that, considering the ages, this massif is sufficiently old compared to the other massifs, especially Mount Manengouba, because these acid magmas, according to [62], require a significant period of time for their formation to be elaborated.
\nCalderas are places where several natural hazards occur, including volcanic eruptions and mass movements [63, 64]. According to [65], calderas are destructive volcanic forms because they cause pre-existing reliefs to collapse, unlike post-caldera cones and domes, which are constructive because pre-existing reliefs are put in place. Moreover, the volcanic formations that cover them favor the formation of fertile soils and the development of a plant cover of various species conducive to an agropastoral activity [16]. These are environments where hydrothermal activities and mineralization processes generally occur [57, 66, 67]. In this respect, it is clear that calderas have a strong educational value as they allow us to understand the complexity of certain craters in volcanic environments around the world. As such, they allow us to understand the degree of fracturing of the ante-caldera substratum, the superposition of eruptive products and the slices of the flows at the ramparts and the post-eruptive geological processes. For this reason, calderas have been the subject of several studies in the field of geological heritage, notably the Mount Teide caldera in Spain, Aso caldera in Japan; Santorini caldera in Greece; Erta Alé and Fentale caldera in Ethiopia; Cha Das caldera in Cape Verde; Eboga, Santa Mbu, Lefo and Bambouto caldera in Cameroon [17, 68, 69, 70, 71, 72]. Thus, calderas are often the seat of later volcanic activities that leave exceptional geomorphological units with several values suitable for geotourism [33, 51, 52, 56, 73, 74, 75].
\nThe Caldera of Mount Bambouto is a volcanic unit that formed at a period between 18.68 and 22 Ma. Its emplacement model is comparable to that of Cole et al. 2005. Its formation and evolution gave it a rather varied petography and a characteristic structure. Its classification according to the Caldeira DataBase of Geyer and Marti (2008) allows us to conclude that its type of collapse is piecemeal. Chemically, the caldera is alkaline with codes ALKAf, ALKAi, and ALKAm. Furthermore, this caldera was formed through a continental rifting of extensional type, and their postcaldera protrusions give them Type-S and Type-MS. Moreover, it is a well-preserved caldera because its ridge lines are well observable.
\nThe classification of the caldera of Mount Bambouto made within the framework of this work makes it possible to understand the similarities of this caldera with other calderas around the world on the one hand and to understand part of the global dynamics of the functioning of the Cameroon Volcanic Line on the other hand. Furthermore, this study contributes to elucidate the origin of the Cameroon Volcanic Line, which is still a subject of discussion among Cameroonian and foreign researchers today. Moreover, through this work, the Mount Bambouto Caldera is promoted next to the world scientific community that is still ignoring his existence.
\nIntechOpen publishes different types of publications
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\\n\\nCompacts provide a mid-length publishing format that bridges the gap between journal articles, book chapters, and monographs, and cover content across all scientific disciplines.
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\n\nEdited Volumes can be comprised of different types of chapters:
\n\nRESEARCH CHAPTER – A research chapter reports the results of original research thus contributing to the body of knowledge in a particular area of study.
\n\nREVIEW CHAPTER – A review chapter analyzes or examines research previously published by other scientists, rather than reporting new findings thus summarizing the current state of understanding on a topic.
\n\nCASE STUDY – A case study involves an in-depth, and detailed examination of a particular topic.
\n\nPERSPECTIVE CHAPTER – A perspective chapter offers a new point of view on existing problems, fundamental concepts, or common opinions on a specific topic. Perspective chapters can propose or support new hypotheses, or discuss the significance of newly achieved innovations. Perspective chapters can focus on current advances and future directions on a topic and include both original data and personal opinion.
\n\nINTRODUCTORY CHAPTER – An introductory chapter states the purpose and goals of the book. The introductory chapter is written by the Academic Editor.
\n\nMonographs is a self-contained work on a particular subject, or an aspect of it, written by one or more authors. Monographs usually have between 130 and 500 pages.
\n\nTYPES OF MONOGRAPHS:
\n\nSingle or multiple author manuscript
\n\nCompacts provide a mid-length publishing format that bridges the gap between journal articles, book chapters, and monographs, and cover content across all scientific disciplines.
\n\nCompacts are the preferred publishing option for brief research reports on new topics, in-depth case studies, dissertations, or essays exploring new ideas, issues, or broader topics on the research subject. Compacts usually have between 50 and 130 pages.
\n\nCollection of papers presented at conferences, workshops, symposiums, or scientific courses, published in book format
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