Yap Trench Research Articles

A Steep Slab at the Yap Trench Resulted from Subducting Oceanic Plateaus

Abstract Interaction of oceanic plateaus with trenches plays a vital role in subduction activities and tectonic evolutions. The Yap trench is a rare case of an oceanic plateau subduction system. However, the knowledge of the impacts of plateau-trench interaction on subduction activity is still insufficient, due to a lack of seismological observations. Using ocean-bottom seismometer data near the Yap trench from April 2016 to May 2017, we conduct seismicity analyses in the Yap subduction zone by utilizing a machine-learning algorithm and matched-filter detections. The pattern of seismicity in the Yap trench exhibits characteristics similar to typical active subduction zones. The seismicity delineates a steep subducting slab, which may have resulted from the blocking of the buoyant Caroline Plateau. The majority of earthquakes are shallower than 80 km in the event-detectable area in the Yap trench, much shallower than the potential slab depth of 350 km from the previous seismic tomography images.

The Impact of the Caroline Ridge Subduction on the Geomorphological Characteristics of Major Landforms in the Yap Subduction Zone

The Caroline Ridge (CR) subduction underneath the Philippine Sea Plate brings complex morphotectonic characteristics to the Yap Subduction Zone (YSZ) compared to other normal intra-oceanic subduction systems. However, due to the relative paucity of precise geomorphological information, the detailed morphotectonic settings of the YSZ remain unclear. Therefore, we combine the latest-released bathymetry, marine geomorphometry techniques, and geophysical information to investigate the geomorphological characteristics of landforms in the YSZ and their inter-relationship with the CR subduction. The Parece Vela Basin displays NE-SW oriented fractures which are believed to be influenced by the subduction of CR in the ESE-WNW direction. The north part of the Yap arc exhibits higher Bouguer anomalies, implying the absence of the overlying normal volcanic arc crust. The arc-ward trench shows abnormal higher slope values and reveals two significant slope breaks. The Yap Trench axis reveals varying water depths with an extraordinarily deep point at around 9000 m. The sea-ward trench slope displays higher slope values than normal and shows the presence of grabens, horsts, and normal faults which indicate the bending of the CR before subduction. The CR subduction is observed to be critical in the formation of significant geomorphological characteristics in the YSZ.

The microbiome and its association with antibiotic resistance genes in the hadal biosphere at the Yap Trench

The hadal biosphere, the deepest part of the ocean, is known as the least-explored aquatic environment and hosts taxonomically diverse microbial communities. However, the microbiome and its association with antibiotic resistance genes (ARGs) in the hadal ecosystem remain unknown. Here, we profiled the microbiome diversity and ARG occurrence in seawater and sediments of the Yap Trench (YT) using metagenomic sequencing. Within the prokaryote (bacteria and archaea) lineages, the main components of bacteria were Gammaproteobacteria (77.76 %), Firmicutes (8.36 %), and Alphaproteobacteria (2.25 %), whereas the major components of archaea were Nitrososphaeria (6.51 %), Nanoarchaeia (0.42 %), and Thermoplasmata (0.25 %), respectively. Taxonomy of viral contigs showed that the classified viral communities in YT seawater and sediments were dominated by Podoviridae (45.96 %), Siphoviridae (29.41 %), and Myoviridae (24.63 %). A large majority of viral contigs remained uncharacterized and exhibited endemicity. A total of 48 ARGs encoding resistance to 12 antibiotic classes were identified and their hosts were bacteria and viruses. Novel ARG subtypes mexFYTV-1, mexFYTV-2, mexFYTV-3, vanRYTV-1, vanSYTV-1 (carried by unclassified viruses), and bacAYTB-1 (carried by phylum Firmicutes) were detected in seawater samples. Overall, our findings imply that the hadal environment of the YT is a repository of viral and ARG diversity.

Quorum Quenching Bacteria Bacillus velezensis DH82 on Biological Control of Vibrio parahaemolyticus for Sustainable Aquaculture of Litopenaeus vannamei

Aquatic pathogens such as Vibrio parahaemolyticus cause a bacterial infection that reduces the economic benefits of aquaculture and affects the food quality and safety of human beings. Quorum quenching (QQ) is considered a novel strategy of microbial antagonism that inhibits pathogens and reduces the abuse of antibiotics. This study investigates a QQ bacterial strain, Bacillus velezensis DH82 from the deep sea Yap trench, in vitro to examine the effects of DH82 and its functional products against V. parahaemolyticus, focusing on the Quorum sensing (QS) regulation and the inhibition of pathogenicity and bacterial growth. The study also conducted in vivo investigation in the aquaculture of Litopenaeus vannamei challenged with V. parahaemolyticus by immersion and injection challenge. The results of the QS regulator transcription level demonstrated the multiple QQ enzymes in DH82 regulated the pathogenicity but could not fully control the biofilm formation; the effective antibacterial activity of extracellular peptides on microbial antagonism verified the inhibition on bacterial growth of V. parahaemolyticus. The in vivo experiment in aquaria demonstrated the effective enrichment of DH82 and inhibition of Vibrio in both the aquatic system and the shrimp intestine. The dietary DH82 relieved the negative effect of Vibrio on the activity of enzyme acid phosphatase (ACP), alkaline phosphatase (AKP), superoxide dismutase (SOD) under challenge of Vibrio pathogens, and was not harmful to host according to lysozyme (LZM) activity. DH82 also ameliorated the damage to the intestine and muscles induced by V. parahaemolyticus infection according to tissue imaging. Though DH82 did present some dose-dependent adverse effects to the host, the findings revealed the effective QQ and antibacterial activity of DH82 on emerging biocontrol against V. parahaemolyticus, therefore indicating the potential application of DH82 as a biological control reagent in the sustainable and green production of aquaculture.

The complete genome sequence of Shewanella inventionis D1489 reveals its potential for the production of eicosapentaenoic acid.

Shewanella inventionis D1489, isolated from a marine sediment sample from the Yap trench, is a psychrophile bacterium with optimal and maximum growth temperatures of 17°C and 37°C, respectively. Here, we present the complete genome of Shewanella inventionis D1489, which will facilitate the genome mining of eicosapentaenoic acid (EPA) biosynthesis coding gene cluster. The sequenced genome consists of 4,831,636 bases, with mean G+C content of 42.404%. A total of 4295 coding genes including 97 tRNAs and 25 rRNA were predicted in the genome. The genome provides basic genetic information for the understanding of its adaptation to cold environment.

Seismic Structure of the Caroline Plateau‐Yap Trench Collision Zone

AbstractCollision of oceanic plateaus with trenches has played a key role in the continental growth and plate tectonic reorganizations throughout the Earth's history. However, the understanding of collision between an initially rifted plateau with a trench is still deficient. Here we conduct the first seismic tomography and receiver function analyses in the Yap subduction zone, western Pacific Ocean, where the initially rifted Caroline Plateau is colliding with the Yap Trench. Our results reveal horizontal and overturned slabs south and north of the Sorol Trough, respectively, which may be caused by slab breakoff followed by underplating and eastward mantle flow with ultra‐slow convergence. The distinct slab morphologies could be responsible for the short‐lived arc volcanism (11‐7 Ma), horst‐graben structures, different Bouguer gravity anomalies and stress regimes in the Yap subduction zone. The overturned slab may cause the incoming plateau to be stretched to facilitate the initial plateau subduction.

Copper Isotopic Fractionation During Seafloor Alteration: Insights From Altered Basalts in the Mariana and Yap Trenches

AbstractTo further investigate copper (Cu) isotopic fractionation during seawater‐oceanic crust interactions, 13 subsamples across a basalt altering section and 12 bulk‐rock basalts from the southern Mariana and Yap trenches, western Pacific Ocean, were studied. We find that the δ65Cu values of the basalt section roughly increase from mid‐ocean ridge basalt‐like values (0.04% – 0.10%) in the core to higher values (up to 0.20%) near the core‐rim interface, and then lower values (down to −0.17%) at the rims. Isotopically light rims reflect the initial dissolution of Cu‐bearing sulfides releasing isotopically heavy Cu into ambient seawater, consistent with both lower Cu and sulfide contents in the altered rims. The elevated δ65Cu values reveal that sulfide dissolution induced a concentration‐driven diffusion from the core to rims, controlling the rim‐core‐rim Cu content and isotopic variations on centimeter scale. By contrast, the δ65Cu values of bulk‐rock basalts show a wide range (0.02% – 0.56%) with most samples enriched in heavy isotopes, and negatively correlate with Cu concentrations, indicating preferential adsorption of isotopically heavy Cu from seawater. We propose that chemical diffusion occurred prior to any adsorption processes, suggesting that a three‐stage process involving sulfide dissolution, chemical diffusion and adsorption controls Cu isotopic fractionation during seafloor basalt alteration.

The cold adaption profiles of Pseudoalteromonas shioyasakiensis D1497 from Yap trench to cope with cold

Genome sequencing of Pseudoalteromonas shioyasakiensis D1497, a psychrophile from the Yap trench, revealed that it contained a circle chromosome of 3,631,285 bp with 40.94% GC content and prefered to use codons with A/T in the third position. Additionally, the relative synonymous codon usage (RSCU) values indicated the codons with A and T in the third position were always the most used. Cultivation of P. shioyasakiensis D1497 presented lower substrate consumption rate, higher ATP pool and higher conversion rate of biomass per unit substrate consumed at low temperature (15 °C) than that of the room temperature (25 °C) culture. Comparative transcriptomic analysis revealed that the mRNA abundance of energy metabolism related genes was decreased in 15 °C culture compared with that of 25 °C culture. In addition to its codon usage biases profile, P. shioyasakiensis D1497 presented an energy saving metabolism strategy to cope with cold, converting more carbon source into biomass in cold environment.

The Sources of Organic Carbon in the Deepest Ocean: Implication From Bacterial Membrane Lipids in the Mariana Trench Zone

Hadal trenches have higher microbial carbon turnover rates as compared to adjacent abyssal plains. However, the source of organic carbon in the trench remains enigmatic. In this study, we show that a fraction of organic carbon is possibly derived in situ and correlated with chemoautotrophic communities supported by the fluid discharge of water-rock interaction in the trench wall, based on analysis of glycerol dialkyl glycerol tetraether (GDGT) membrane lipids, including archaeal isoprenoid GDGTs (IsoGDGTs) and bacterial branched GDGTs (BrGDGTs), in sediments and rocks of the Mariana and Yap Trenches, northwest Pacific Ocean. These trench sediments contained relative higher BrGDGTs ratios, which was a rare observation in the open ocean. The BrGDGT-to-IsoGDGT ratios ranged in 0.02–0.88 (mean = 0.10 ± 0.11) in sediments and 0.09–0.38 (mean = 0.17 ± 0.13) in altered rocks. The calculated values of branched and isoprenoid tetraether (BIT) index ranged from 0.02–0.73 (mean = 0.18 ± 0.11) in sediments and from 0.16–0.9 in altered rocks (mean = 0.37 ± 0.27). Moreover, these GDGTs exhibited similar characteristics to those of altered basalt rocks, indicating inputs of organic carbon from the trench subsurface environment. Thus, in addition to organic-rich material settling, we propose chemoautotrophic activity in oceanic crust could be an additional source of organic carbon in the deepest part of the ocean, with an important role in deep-sea carbon cycles.

Fungal Diversity in Deep Sea Sediments from East Yap Trench and Their Denitrification Potential

In recent years, the hadal trenches have been recognized as biological hot spots for deep sea researchers. Due to high hydrostatic pressure, low temperatures, high salinity and low nutrients, the microorganisms in hadal trenches may have unique community structure with potential for biotechnical application. Compared with bacteria and archaea, the diversity and ecological roles of fungi in hadal trenches remain largely unknown. The purpose of this study was to explore fungal diversity in deep-sea sediments of the Yap trench and their denitrification potential. In the present study, a total of 106 fungal strains were isolated from six sediment samples collected in the East Yap Trench. These fungi belonged to five classes (Dothideomycetes, Eurotiomycetes, Sordariomycetes, Cystobasidiomycetes, and Microbotryomycetes), thirteen genera (Acremonium, Alternaria, Aureobasidium, Aspergillus, Cladosporium, Cystobasidium, Engyodontium, Gliomastix, Lecanicillium, Penicillium, Phoma, Rhodotorula and Trichoderma) and eighteen species, based on morphological identification and ITS-rDNA sequence analysis. Among them, the dominant genus is Cladosporium, which accounting for 42.45% of the total fungal strains. Meanwhile, the denitrification potential of the fungal strains was also examined with two different denitrifying media (nitrate and nitrite as sole substrate, respectively). Two fungal strains (Acremonium sp. and Aspergillus versicolor), were found to be able to produce N2O ex situ in the presence of nitrite. No fungus was found to produce N2O by using nitrate. Our results suggest that fungi in hadal sediments, play important roles in nitrogen cycles.

Characteristics and implications of isoprenoid and hydroxy tetraether lipids in hadal sediments of Mariana and Yap Trenches

As one of the least-explored regions on Earth, the hadal zone remains poorly understood in terms of sedimentary organic geochemistry. This study examined the composition of isoprenoid glycerol dialkyl glycerol tetraethers (Iso-GDGTs) and hydroxy GDGTs (OH-GDGTs) in sediment cores with water depths ranging from 5058 to 10,911 m from the Mariana and Yap Trenches. The results showed a higher proportion of GDGT-0 (25–73%, mean = 49%) in the trench Iso-GDGTs pool than those from shallower ocean counterparts (<5000 m). Properties, including higher values of the [GDGT-2/GDGT-3] ratio (7.17–20.03, mean = 13.02) and the [GDGT-0/Crenarchaeol] ratio (0.49–3.94, mean = 1.48), as well as a dominance of OH-GDGT-0 in the OH-GDGTs, are similar to characteristics observed in other cold deep marine environments rather than tropical shallow ocean. Ring Index decreased with increasing water depth of the sampling sites, corresponding with increased fractional abundance of acyclic Iso-GDGTs and OH-GDGTs. Paleothermometer TEX86 in the surface sediments (>5000 m) revealed a significant negative linear correlation with water depth (TEX86H: R2 = 0.89, p < 0.01; TEX86L: R2 = 0.89, p < 0.01), leading to a bias toward lower proxy-derived temperatures. This is likely due to the increased incorporation of cold- and pressure- adapted species of archaea in dark ocean. Overall, this study provided implications of the extreme water depth effect on the distribution of isoprenoid and hydroxy tetraether lipids, as well as the proxy application in hadal environments.

Geochemical and chronological evidence for collision of proto-Yap arc/Caroline plateau and rejuvenated plate subduction at Yap trench

The Yap Arc was considered to have derived from the proto-Yap-Izu Bonin-Mariana arc system. It is a rare example of subduction of an oceanic plateau with short arc–trench distance and consists mainly of metamorphic rocks, which are distinct from the Izu Bonin-Mariana arc system. However, it is not known on the origin and formation time of the basement rocks of the Yap Arc. For the first time, in this study we provide the results of radiometric age-dating and whole-rock major element, trace element and Sr–Nd–Pb–Hf isotope analyses for the metamorphic basement rocks (amphibolites) of the Yap Arc. These rock samples can be classified into three groups based on their major and trace element compositions. Group 1 samples have strong depletion of LREEs and a Dupal-type isotopic signature, and they represent forearc basalts (FABs) of the nascent Yap forearc. Group 2 samples have an alkali basalt-like geochemistry and oceanic island basalts (OIBs) type trace element patterns, and they represent the basalts of the Caroline Plateau. Group 3 samples have island-arc-type negative anomalies of Nb–Ta–Zr–Hf, and they may represent the volcanic rocks of the proto-Yap Arc. These amphibolites were formed at 21 Ma according to 40Ar/39Ar amphibole dating and in situ SIMS UPb titanite dating, and they record the timing of the collisional event between the Caroline Plateau and the proto-Yap Arc. We propose that the Yap arc has been evolving distinctly from the Izu-Bonin-Mariana Arc since this collision time. These rocks were metamorphosed and brought onto the present Yap Arc as a result of the collision between the proto-Yap Arc and the Caroline Plateau. Based on the new results of age-dating and geochemistry of this study, we propose three stages of tectonic evolution for the Yap Arc as a result of collision from the Caroline plateau: an early stage (proto-Yap Arc) of subduction of the Caroline Plate, collision of the proto-Yap Arc with the in-coming young Caroline Plateau, and rejuvenated plate subduction at the Yap Trench with limited volcanism.

Spatial heterogeneity of organic carbon cycling in sediments of the northern Yap Trench: Implications for organic carbon burial

The hadal trenches (>6000 m) are considered to be ultimate sinks of organic carbon (OC) from biosphere. However, highly spatial heterogeneity of geographic background and organic matter in different zones make significant influences on the OC cycling, and further the carbon burial. In this study, three sediment cores were drilled across the northern Yap Trench axis (9.8–9.9°N, 138.3–138.7°E). The elemental compositions, stable carbon isotopes of organic matter, mineral-specific surface area, and grain size composition were analyzed to investigate the spatial variations of organic sources, distribution, and its degradation in the northern Yap Trench. The surface sedimentary OC (SOC) contents in the northern Yap Trench increase from 0.25% at abyssal depth (4435 m) to 0.50% at hadal depth (~6674 m). Higher OC content (0.27% ± 0.08%) and sedimentation rate (5.8 cm kyr−1) occur in the station on the gradual oceanward slope (~4.2°) compared to those on the steep landward slope (~10°) (0.17% ± 0.13%, 0.52–1.8 cm kyr−1), suggesting enhanced accumulation of OC on the gradual slope. The allochthonous OC (i.e. marine phytoplankton-derived (55% ± 7%) and terrestrial (16% ± 8%)) dominates the SOC pool on the oceanward slope, whereas autochthonous microbe reworked OC contributes more than 50% in the steep landward slope, based on the evaluation of a three-end-member mixing model using δ13C composition and OC/N ratios as source markers. Correspondingly, radiocarbon age of SOC in the gradual slope is ~700 years younger than that in the steep slope with similar depth, indicating that the relatively fresh allochthonous OC is selectively deposited on the gradual slope. A multi-G degradation model demonstrates that OC degradation rates in the northern Yap Trench range from 0.00015 yr−1 to 0.00068 yr−1, which can be comparable with abyssal plain (3000–6000 m) and are lower than those of neritic environments (<1000 m). Mass accumulation model calculation shows that accumulation rate of surface OC in the northern Yap trench is ~2.7 × 10−2 g C m−2 yr−1, much lower than those from other deep ocean seafloors. This study suggests an inefficient SOC preservation within the northern Yap Trench, which might be induced by high labile marine phytoplankton-derived OC inputs and active heterotrophic microbial activity, and the results have important implications for better understanding the effects of sediment dynamics on OC cycling in hadal zones.

Genomic Characterization of a Novel Gut Symbiont From the Hadal Snailfish.

Hadal trenches are characterized by not only high hydrostatic pressure but also scarcity of nutrients and high diversity of viruses. Snailfishes, as the dominant vertebrates, play an important role in hadal ecology. Although studies have suggested possible reasons for the tolerance of hadal snailfish to high hydrostatic pressure, little is known about the strategies employed by hadal snailfish to cope with low-nutrient and virus-rich conditions. In this study, the gut microbiota of hadal snailfish was investigated. A novel bacterium named “Candidatus Mycoplasma liparidae” was dominant in the guts of three snailfish individuals from both the Mariana and Yap trenches. A draft genome of “Ca. Mycoplasma liparidae” was successfully assembled with 97.8% completeness by hybrid sequencing. A set of genes encoding riboflavin biosynthesis proteins and a clustered regularly interspaced short palindromic repeats (CRISPR) system was present in the genome of “Ca. Mycoplasma liparidae,” which was unusual for Mycoplasma. The functional repertoire of the “Ca. Mycoplasma liparidae” genome is likely set to help the host in riboflavin supplementation and to provide protection against viruses via a super CRISPR system. Remarkably, genes encoding common virulence factors usually exist in Tenericutes pathogens but were lacking in the genome of “Ca. Mycoplasma liparidae.” All of these characteristics supported an essential role of “Ca. Mycoplasma liparidae” in snailfish living in the hadal zone. Our findings provide further insights into symbiotic associations in the hadal biosphere.

Geochemical characteristics of hadal sediment in the northern Yap Trench

Two sediment cores were retrieved in the hadal zone of the Yap Trench, and their concentrations of six major elements Mg, Al, Ca, Ti, Mn and Fe and nine trace elements Sr, Ba, Pb, V, Cr, Co, Ni, Cu and Zn were determined in inductively coupled plasma atomic emission spectrometry (ICP-AES). According to the vertical distribution profiles of the 15 elements, the correlation of their concentrations, the ratios of Ni/Co, V/Cr, Fe/Al, and Ti/Al, and morphological characteristics of the sediment samples, the implications of the depositional environment and the sediment provenance were analyzed. The results show that the ratio of Ni/Co in all depths of the two sediment cores were below 5, and the ratio of V/Cr were lower than 2, indicating that the depositional environment of the hadal zone in the trench was oxidative and might have inflow of the Antarctic bottom oxygen-rich water. The sediment samples on the eastern side of the trench were siliceous mud mainly composed of diatoms, radiolarian, and sponge needles from surface to deep layer. The vertical profile of the elements, the concentration of TOC and the fossil record indicated that the sediment sample from station Dive113 was well mixed from surface to bottom layer. Based on the correlation of concentrations of the elements, the morphological characteristics of the sediment, and the ratios of Fe/Al and Ti/Al, we inferred that the sediment in the hadal zone of the trench had terrestrial, volcanic, biological, and authigenic sources. Major source of the sediment in the eastern side of the trench were terrestrial; whereas the sediment in the western side of the trench received more volcaniclastic input.

Water characteristics of abyssal and hadal zones in the southern Yap Trench observed with the submersible Jiaolong

Using observations in an applied cruise of the submersible Jiaolong, water characteristics, geostrophic transport, and turbulent mixing in abyssal and hadal zones of the southern Yap Trench were studied. The spatial structures of deep water show that the abyssal water is cold, saline, and oxygen rich. The hadal water has very small changes in potential temperature and potential density, and a little decrease in salinity and obvious decrease in oxygen. The isotherm, isopycnal, and isohaline are depressed in abyss over the central trench. The turbulent mixing is enhanced in the near-bottom zone and the hadal water on the trench slope, especially at the steep slope, the dissipation rate and diffusivity is strong, which weakens the stratification. The geostrophic flows move southward in the western region of the trench and northward in the eastern region, indicating cyclonic circulation. In the central region of the trench, the water transport is ~1.74 Sv southward. In the hadal zone, the northward and southward transports are balanced. Our analysis suggests that the abyssal water in the southern Yap Trench is from Lower Circumpolar Water (LCPW) and the hadal water seems to be of the isolated local water rather than LCPW.

Subduction Erosion, Crustal Structure, and an Evolutionary Model of the Northern Yap Subduction Zone: New Observations From the Latest Geophysical Survey

AbstractThe Yap subduction zone is a distinctive erosive margin with an extremely slow convergence rate. The high relief of the subducting plate, generated by horst and graben structures and seamounts, leads to attenuation of the crust. In this study, we present the latest geophysical data, collected by the Chinese research vessel Kexue, to investigate subduction erosion at the Yap subduction zone and develop subduction models for Yap subduction zone structures. We show an anomalous distance between the Yap Trench and the adjacent volcanic arc, the steep slope of the trench arcward, a frontal prism, and rare sediment in the trench, all typical features of erosive margins. We propose that the high‐relief subducting plate has led to erosion of the overlying plate and that different subduction processes, controlled locally by the topography of the subducting plate, have modified the Yap subduction zone. Numerous normal faults increase the relief of the seafloor entering the trench, and an anomalously large slope angle along the trench reflects uplift of the fore‐arc high via seamount subduction. In addition, the thin crust of the subducted horst and graben structures, along with the normal faults, might have eroded the fore‐arc crust and subsequently eroded the Yap arc crust during subduction. These subduction erosional processes at the Yap Trench provide one of the best cases of an erosive margin in the world, particularly for a subduction zone with an extremely slow convergence rate.

Origin of the Palau and Yap trench-arc systems

SUMMARY This paper attempts to account for several unique morphological and geological characteristics of the Palau and Yap trench-arc systems in the northwestern Pacific Ocean using a new hydrodynamic model postulated herein. The model is a simple mathematical treatment of a stationary viscous flow pattern in the asthenosphere that causes an appreciable amount of mechanical resistance against a vertically subducted rigid slab moving horizontally together with the flat plate. A couple of thrusting forces comprising uplifting pressure generated in the frontal edge of the overriding lid and a new type of tectonic erosion along the surface of the vertical slab seem to reasonably explain apparently contradictory features of the Palau and Yap trench arcs. Long-term GPS measurements show that the Palau and Yap trench arcs are moving over the viscous asthenosphere toward the NWW with velocities as great as 10 cm yr −1 . Stresses along the trench arcs predicted by the model would be sufficiently large to maintain their present morphology: (1) water depths greater than 8000 m in spite of the extremely small plate convergence rates and relatively young ages of subducted plate; (2) V-shaped cross-section of the axial bottom of these trenches, implying little cover of slumped deposits in spite of very steep landward slopes; (3) serpentinized peridotites, gabbros, basalts and limestones are exposed on the landward slope with neither sediment cover nor ferromanganese hydro-oxide coatings; (4) abnormally close proximity of the Palau and Yap islands to the trench axis; (5) predominant distribution of barrier reefs in their western periphery apparently opposite to the easterly to northeasterly prevailing wind.

Deformation from the convergence of oceanic lithosphere into Yap trench and its implications for early-stage subduction

The surface expression generated by convergence of two oceanic plates and sinking of the older lithosphere into the mantle is one of the most spectacular features of our planet, and yet very little is understood about the onset of this dynamic process. This is largely due to the lack of modern-day analogues where causal relationships among various subduction parameters can be investigated. Here we report a rare example in the western Pacific where variations in style of deformation and state of stress are observed on a young trench-arc system as a result of subduction of the Oligocene Caroline plate beneath the Philippine Sea plate along the Yap Trench. The unique features of this system include a short trench-arc distance (∼50 km), narrow trench (<50 km), and the presence of the Caroline Ridge, a region of massive volcanic outflow formed on the subducting Caroline plate, which is divided into two by the Sorol Trough trending WNW–ESE. While the timing of collision is uncertain and the possible rejuvenation of an old subduction zone can not be ruled out, the convergence apparently changed to subduction when the Caroline plate reached the mechanically weak part of the overriding plate. The style of deformation changes at approximately 9°N, which corresponds to the southern border of the Sorol Trough. To the north, the area is generally characterized by extensional features on the arc and slab with a large half graben (100 km×50 km) on the plate entering the subduction zone. To the south, compression is the dominant mode of deformation on the arc and slab. The average depth of the subducting plate to the north lies 500 m higher than to the south, and this height appears to be maintained by broad flexural bending applied by the Yap and southern Mariana Trenches. Although the convergence rate is higher to the north of Sorol Trough than the south, the gravity anomalies show that the slab has advanced deeper into the asthenosphere to the south, which is interpreted as evidence that subduction started later to the north than south. The study also reveals that during the initial early stage of subduction a broad flexure may develop on the slab, but with further convergence, the deformation is localized and the slab is deflected at the maximum bending point.

Morphology and tectonics of the Yap Trench

We conducted swath bathymetry and gravity surveys the whole-length of the Yap Trench, lying on the southeastern boundary of the Philippine Sea Plate. These surveys provided a detailed morphology and substantial insight into the tectonics of this area subsequent the Caroline Ridge colliding with this trench. Horst and graben structures and other indications of normal faulting were observed in the sea-ward trench seafloor, suggesting bending of the subducting oceanic plate. Major two slope breaks were commonly observed in the arc-ward trench slope. The origin of these slope breaks is thought to be thrust faults and lithological boundaries. No flat lying layered sediments were found in the trench axis. These morphological characteristics suggest that the trench is tectonically active and that subduction is presently occurring. Negative peaks of Bouguer anomalies were observed over the arc-ward trench slope. This indicates that the crust is thickest beneath the arc-ward trench slope because the crustal layers on the convergent two plates overlap. Bouguer gravity anomalies over the northern portion of the Yap Arc are positive. These gravity signals show that the Yap Arc is uplifted by dynamic force, even though dense crustal layers underlie the arc. This overlying high density arc possibly forces the trench to have great water depths of nearly 9000 m. We propose a tectonic evolution of the trench. Subduction along the Yap Trench has continued with very slow rates of convergence, although the cessation of volcanism at the Yap Arc was contemporaneous with collision of the Caroline Ridge. The Yap Trench migrated westward with respect to the Philippine Sea Plate after collision, then consumption of the volcanic arc crust occurred, caused by tectonic erosion, and the distance between the arc and the trench consequently narrowed. Lower crustal sections of the Philippine Sea Plate were exposed on the arc-ward trench slope by overthrusting. Intense shearing caused deformation of the accumulated rocks, resulting in their metamorphism in the Yap Arc.