Research Article
Research Article
A new genus and species of Thyasiridae (Mollusca, Bivalvia) from deep-water, Beaufort Sea, northern Alaska
expand article infoPaul Valentich-Scott, Charles L. Powell II, Thomas D. Lorenson, Brian E. Ewards
† Santa Barbara Museum of Natural History, Santa Barbara, United States of America
‡ U.S. Geological Survey, Menlo Park, United States of America
Open Access


Bivalve mollusk shells were collected in 2350 m depth in the Beaufort Sea, Arctic Ocean off northern Alaska. Initial identification suggested the specimens were a member of the bivalve family Thyasiridae, but no known eastern Pacific or Arctic living or fossil thyasirid resembled these deep-water specimens. Comparisons were made with the type of the genera Maorithyas Fleming, 1950, Spinaxinus Oliver & Holmes, 2006, Axinus Sowerby, 1821, and Parathyasira Iredale, 1930. We determined the Beaufort Sea species represents a new genus, herein described as Wallerconcha. These specimens also represent a new species, herein named Wallerconcha sarae. These new taxa are compared with known modern and fossil genera and species of thyasirds.


Thyasiridae, Beaufort Sea, Alaska, Mollusca, Bivalvia, Maorithyas, Wallerconcha, Spinaxinus, Axinus, Parathyasira, chemoautotrophic, endosymbiosis, taxonomy, Arctic Ocean


In an effort to understand the tectonic and sedimentary history of the Arctic Ocean between Canada and Alaska, a joint US-Canadian ice breaker expedition working under the sponsorship of the Extended Continental Shelf Project conducted operations in the Canada Basin during August 2010. The primary mission of the expedition was to collect seismic-reflection and high-resolution bathymetric data. Occasionally there was an opportunity to collect gravity and piston core samples throughout the basin. One of these cores was collected on a mound previously identified on seismic records. Bivalve mollusk specimens were collected in some of these samples and have provided the material for this paper.

Geologic setting

The informally named “Canning Seafloor Mound” (Hart et al. 2011; hereafter referred to as the Canning Seafloor Mound), a probable cold seep, overlies the crest of a buried anticline in a region of sub-parallel compressional folds beneath the eastern Beaufort Sea outer slope. The collecting locality is adjacent to the frontier oil and gas regions offshore of Prudhoe Bay. The basin is host to extraordinarily deep sedimentary sections about 10 km thick with high organic matter content from river discharge, enhancing the probability of oil and gas generation at depth (Grantz et al. 2011, Grantz and Hart 2012).

Taxonomic background

Bernard (1972) reviewed the thyasird bivalves in western Canada. He examined specimens from throughout the northeast Pacific as well in the Arctic. In this treatment he synonymized a large number of genera into Thyasira Lamark, 1818, including Axinus G.B. Sowerby I, 1821 and Conchocele Gabb, 1866. Both genera are now known to be distinct (Oliver and Holmes 2007; Coan and Valentich-Scott 2012).

The only systematic treatment that included deep-water Beaufort Sea bivalves was presented by Bernard (1979). In the Beaufort Sea he documented four species of Thyasiridae between the intertidal zone and 2560 m, including a minute deep-water species Axinulus careyi Bernard, 1979.

Kristofovich (1936) reported on the Thyasira of Tertiary deposits on the western coast of Kamchatka, Russia. Fossil and modern species of Thyasira from northeastern Honshu, Japan, were detailed by Yabe and Nomura (1925).

Considerable research has been published in the last 15 years on thyasirds from cold seeps and hot vents (Oliver and Sellanes 2005, Oliver and Holmes 2006, 2007b, Oliver and Levin 2006, Taylor et al. 2007, Zelaya 2009, Oliver et al. 2013, Hryniewicz et al. 2014, Oliver 2014) and their associated with chemosynthetic communities, which are now known to be distributed widely throughout the world’s oceans (Sibuet and Olu 1998, Fujikura et al. 1999, Fujiwara et al. 2001). The Canning Seafloor Mound probably represents a cold seep habitat (Hart et al. 2011).

Here we describe a new genus and new species of thyasirid bivalve from a deep-water seafloor mound in the eastern Beaufort Sea, off northern Alaska and compare it to other thyasirid genera and species.

Materials, methods, abbreviations

Bivalve specimens were examined from cores collected by the USCGC Healy (cruise HLY1002; USGS Station FAID H–3–10–AR; 71.3176°N, 143.9982°W) from the Canning Seafloor Mound, at a depth of 2530 m in the Beaufort Sea off northern Alaska (Figure 1). The Canning Seafloor Mound is conical and approximately 1200 m diameter and 180 m high (Figure 2).

Figure 1.

Base map adapted from Jakobsson et al. (2008) showing the location of the Canning Seafloor Mound off the coast of northern Alaska.

Figure 2.

Shaded seafloor bathymetry showing shape and approximate dimension of the Canning seafloor mount. The core sites are shown as red dots.

The bivalve specimens were recovered in two cores (1P–1 and 1GB–1) from 0.02 to 4.65 meters below the seafloor. The greater depth indicates long-term residence of the bivalves (see below under Age), whereas the shallow depth and assumed young age could indicate that this species might still be living on or near the mound. The shells are associated with gas hydrate, methane saturated sediments and authigenic carbonates (Edwards et al. 2011, Hart et al. 2011, Lorenson et al. 2011, Pohlman et al. 2011). This strongly suggests that the bivalves had chemotrophic endosymbionts similar to other bivalves that inhabit active cold vents (Roberts and Carney 1997, Fujiwara et al. 2001, Oliver 2014).

For Figure 7, diagrammatic line drawings were made from digital images of the holotypes of each species. Outlines of each type specimen were made in Adobe Photoshop by selecting all space outside of the shell, inversing the selection and creating a clipping path along the shell edge. With the clipping path selected, we processed the “stroke path” command.

The following abbreviations are used in the text: ECS – Extended Continental Shelf; FAID – field activity identification; GNS – GNS Science, Lower Hutt, New Zealand; LACMIP – Invertebrate Paleontology section, Natural History Museum of Los Angeles County, California, USA; mbsf – meters below seafloor; SBMNH – Santa Barbara Museum of Natural History, California, USA; NHMUK – The Natural History Museum, United Kingdom; NMST – National Museum of Nature and Science, Tokyo, Japan; NMW.Z – National Museum of Wales, Zoology, Cardiff, Wales, UK; USGS – United States Geological Survey; USNM – National Museum of Natural History, Smithsonian Institution, Washington D.C., USA.

Systematic account

Family Thyasiridae Dall, 1900

Wallerconcha Valentich-Scott & C. L. Powell, gen. n.

Figures 3A–H, 7B

Type species

Wallerconcha sarae Valentich-Scott & C.L. Powell, new species herein (Figures 3A–H, 7B). No other species are currently included in the genus.

Figure 3.

A–H. Wallerconcha sarae gen. n., sp. n. A–H holotype, SBMNH 235481, length = 23.9 mm, height = 21.3 mm, width = 16.7 mm. A Exterior of right valve B Exterior of left valve C Dorsal view of both valves D Close up of periostracum of right valve E Interior of left valve F Interior of right valve G Close up of hinge of left valve H Close up of hinge of right valve.


Shell moderate in size (length to 24 mm), subtrigonal, subequilateral, strongly inflated; beaks broad, strongly prosogyrous; posterior radial sulcus shallow; sculpture of moderate to strong, uneven commarginal ribs and striae; periostracum thick, dehiscent, medium to dark brown, wrinkled, without micro-spines; lunule absent; escutcheon long, moderately narrow, moderately impressed; ligament large, long, deeply sunken on a stout nymph; hinge edentulous or with minute tubercles; hinge fig well defined and strongly thickened posteriorly; anterior adductor muscle scar wide, long.


The genus is named in honor of Thomas R. Waller (Smithsonian Institution) for his significant contributions to our understanding of the evolution, biogeography and systematics of fossil and modern marine bivalves.


Wallerconcha differs from all other members of the Thyasiridae by the combination of four primary shell characteristics: 1) a well-defined hinge fig; 2) a heavy, deeply sunken nymph; and 3) a broad, elongate anterior adductor muscle scar that is not divided into two sections; 4) a dark, thick, wrinkled periostracum, without micro-spines.

Wallerconcha is similar to the deep-water genus Spinaxinus Oliver & Holmes, 2006 (type species, Spinaxinus sentosus Oliver & Holmes, 2006) (Figure 4A–D). The latter genus has a thin, translucent, minutely spinose periostracum (Figure 4D), whereas the periostracum of Wallerconcha is thick and wrinkled but lacks periostracal spines (Figure 3D). In addition, Wallerconcha has a much longer and wider anterior adductor muscle scar, and a longer and deeper nymph.

Another similar genus is Axinus G.B. Sowerby I, 1821 (type species Axinus angulatus G.B. Sowerby I, 1821). Oliver and Holmes (2007a) reviewed several members of this genus and concluded that it has a large lunule, a moderate to strong posterior radial sulcus, a thin hinge fig, and lacks a heavy nymph, all features which separate it from Wallerconcha.

Parathyasira Iredale, 1930 (type species Parathyasira resupina Iredale, 1930) has an external sculpture of minute rows of spines, and a distinct radial sulcus. It also has a thin hinge fig and weak nymph, which are less robust than Wallerconcha. Both genera have an elongate anterior adductor muscle scar, whereas in Parathyasira the scar is usually divided into several sections, Wallerconcha has a single, broad scar.

Figure 4.

A–D Spinaxinus sentosus. A–G holotype, NMW.Z. 2002.108.1, length = 13.5 mm, height = 13.3 mm, width = 8.6 mm. A Exterior of right valve B Interior of left valve C Dorsal view of both valves D Scanning electron micrograph of periostracum, scale bar = 200 µm. Photo credit P. Graham Oliver and Anna M. Holmes, National Museum of Wales.

Maorithyas marama Fleming, 1950, the type species of the genus, has a very thin hinge fig, lacks a heavy nymph, and has a shorter anterior adductor muscle scar (Figures 5A–G, 7A) when compared to Wallerconcha.

Figure 5.

A–G Maorithyas marama, holotype, GNS–TM 305, length = 18.7 mm, height = 17.2 mm, width = 13.7 mm. A Exterior of right valve B Exterior of left valve C Dorsal view of both valves D Interior of left valve B Interior of right valve F Close up of hinge of left valve G Close up of hinge of right valve.

Okutani et al. (1999) placed their new, deep-water Japanese thyasirid species into the shallow-water genus Maorithyas Fleming, 1950. They chose the generic placement of Maorithyas hadalis Okutani et al., 1999 based on the shallow posterior radial sulcus, and relatively heavy sculpture. The internal shell characteristics of M. hadalis (holotype, NSMT 71431), namely the periostracum, hinge fig, nymph and anterior adductor muscle scar place it outside of Maorithyas or Wallerconcha (Figure 6A–H). It potentially belongs in a new genus, but that description is outside the scope of this paper.

Figure 6.

A–H Maorithyas hadalis, holotype, NSMT 71431, length = 26.7 mm, height = 24.1 mm, width = 13.4 mm. A Exterior of right valve B Exterior of left valve C Dorsal view of both valves D Close up of periostracum of right valve E Interior of left valve F Interior of right valve G Close up of hinge of left valve H Close up of hinge of right valve.

Figure 7.

Comparison of adductor muscle scars and pallial lines of left valves of holotypes. A Maorithyas marama, holotype B Wallerconcha sarae, holotype C Spinaxinus sentosus, holotype. – Not to scale.

Wallerconcha sarae Valentich-Scott & C.L. Powell, sp. n.

Figure 3A–H, 7B


Shell shape. Shell subtrigonal, moderately thin, equivalved, highly inflated; anterior margin broadly rounded; posterior end subtruncate; umbo broadly rounded, strongly prosogyrate; dorsal margin strongly sloping on both sides of the umbo; escutcheon moderately narrow, moderately deep, well-defined; lunule absent. Maximum length 24 mm, maximum height 24 mm, maximum width 17 mm.

Sculpture and periostracum. Shell with closely spaced, irregular commarginal striae and ribs; shallow, narrow radial sulcus extends from posterior of the umbo to the posterior ventral margin; shallow radial depression from the umbo to the central ventral margin, forming a slight undulation along the ventral margin; periostracum thick, wrinkled, dehiscent, light to dark brown, silky.

Hinge. Hinge heavy, edentulous, or with minute tubercles under beaks; anterior section narrow; posterior section with wide lateral platform, supporting deeply sunken nymph; ligament external, deeply sunken, long, dark brown.

Adductor muscle and pallial scars – anterior adductor muscle scar large, long, wide, subelliptical, with irregular upper and lower margins, upper margin of scar concave near the center; posterior adductor muscle scar smaller, irregular ovate, with a pointed projection in juveniles; pallial line scalloped, without a sinus.

Interior – interior dirty white to gray; with faint radial crescent-shaped lines that extend from near the umbo to the near the ventral margin, lines have broad depressions between them near the central ventral margin.

Type locality

USA, Alaska, Beaufort Sea, Canning Seafloor Mound. Specifically, 71.317°N, 143.999°W; 2,358 m water depth (ECS004 137, Core IP–1, section 3, 31 cm, 4.65 mbsf).

Type specimens

Holotype – SBMNH 235481, 1 pair, length = 23.9 mm, height = 21.3 mm, width = 16.7 mm. Alaska, Beaufort Sea, Canning Seafloor Mound; 71.317°N, 143.999°W; 2,358 m water depth (ECS004137, Core IP–1, section 3, 31 cm; 4.65 mbsf)

Paratype 1 – CAS paratype 72852

Alaska, Beaufort Sea, Canning Seafloor Mound; 71.317°N, 143.998°W; 2,350 m water depth (ECS 004 122. Core 1GB–1 102 cm, 1.02 mbsf); length = 12.8 mm, height = 10.9 mm

Paratype 2 – LACMIP paratype 14470

Alaska, Beaufort Sea, Canning Seafloor Mound; 71.317°N, 143.999°W; 2,358 m water depth (ECS004242, Core IP1, section 1, 52 cm, 2/2, 0.52 mbsf); length = 15.0 mm, height = 13.1 mm

Paratype 3 – SBMNH paratype 235613

Alaska, Beaufort Sea, Canning Seafloor Mound; 71.317°N, 143.998°W; 2,350 m water depth (ESC004180, Core 1GB–1, 44 cm, 0.44 mbsf); length = 19.2 mm, height = 17.5 mm

Paratype 4 – SBMNH paratype 235614

Alaska, Beaufort Sea, Canning Seafloor Mound; 71.317°N, 143.998°W; 2,350 m water depth (ESC004180, Core 1GB–1, 44 cm, 0.44 mbsf); length = 23.9 mm, height = 23.8 mm.


Named in honor of Sara Powell, of San Jose, California, daughter of Charles L. Powell.


Wallerconcha sarae is presently only known only from the region around the type locality; the Canning Seafloor Mound (71.3175°N, 143.9997°W), Beaufort Sea, Alaska, USA. Given the collection depth of 0.02–4.65 mbsf, we surmise this is a fossil species. However we cannot discount that it could still be living in the region.

Other specimens examined

Piston core: ESC 004112, Core 1P1, section 4, 15 cm, 4.65 mbsf (articulated specimen; frozen for further analysis), ECS 004137, Core 1P1, section 3, 31 cm, 181 mbsf (one articulate specimen (holotype Figure 3A–G), three larger fragments), ESC 004242, 1P1, sec. 1, 52 cm, 0.52 mbsf, (one left valve), ESC 004242, 1P1, sec. 1, 52–54 cm, 0.53 mbsf (seven large fragments), ECS 004242, 1P1, sec. 1, 52–54 cm, 0.53 mbsf (one fragment). Gravity Core: ESC 004115, Core 1GB1, 0.02 mbsf (left valve; used for chemical analysis), ESC 004122, 1GB1, 102 cm, 1.02 mbsf (one small left valve), CS 004180, Core 1GB1, 44 cm, 0.44 mbsf (one articulate specimen, one left valve, two fragments). EESC 004257, Core 1TC1, section 1, 72 cm, 0.72mbsf (two larger fragments).


The new species has shell characteristics closest to Maorithyashadalis Okutani et al., 1999 (Figures 6A–H), collected from over 7,000 m in the Japanese Trench. Wallerconcha sarae is much more inflated, has broader umbones, and a much longer ligament and nymph. When compared to M. hadalis, W. sarae has a much larger, broader, and more elongate anterior adductor muscle scar.

There are also similarities between Wallerconcha sarae and members of the genus Spinaxinus Oliver & Holmes, 2006. However, all of the currently described species in this genus have a minutely spinose periostracum. The eastern Atlantic S. sentosus (Figures 4A–D) is less inflated than W. sarae, has narrower beaks, and a smaller anterior adductor muscle scar (Figure 7C). Spinaxinus emicatus Oliver in Oliver et al., 2013, from the Gulf of Mexico is compressed and circular in outline, has narrow beaks, an evident radial sulcus, and a much shorter nymph when compared to W. sarae. The Fijian S. phrixicus Oliver in Oliver et al., 2013, is also compressed and circular in outline with narrow beaks, but it has a distinctive shell sculpture of commarginal ridges.

The minute deep-water Beaufort Sea thyasirid, Axinulus careyi is much smaller (maximum length 2.7 mm), has a more defined escutcheon, and lacks the broad posterior hinge fig. It also has a relatively short, narrow anterior adductor muscle scar when compared to the long broad scar of W. sarae.

Axinus grandis (Verrill & Smith in Verrill, 1885) and A. cascadiensis Oliver & Holmes, 2007 have a few external similarities to Wallerconcha sarae. Axinus grandis is an Atlantic and Mediterranean species, that is easily separated from W. sarae by its roughly diamond-shaped shell outline. Axinus cascadiensis is known only from a seamount off Oregon (Oliver and Holmes 2007) and the shell outline serves to separate A. cascadiensis from W. sarae. With A. cascadiensis being less inflated, having narrower, more prosogyrate umbos, and a strong anterior protrusion. In addition, the escutcheon of A. cascadiensis is larger and more deeply impressed.

The Cretaceous fossil Thyasira becca cobbani Kauffman, 1967 (pl. 5, f. 34, 35; 1969, pl. 127, f. 20) has a deep radial sulcus and narrow, strongly prosogyrate beaks. Thyasira becca cobbani is known from the western interior of the North America in the Pierre Shale, Upper Cretaceous (Campanian-Maastrichtian) of Pueblo County, Colorado and in the Riding Mountain Formation, Upper Cretaceous (Campanian-Maastrichtian) exposed along the Assiniboine River, Manitoba, Canada. Thyasira alaskensis Kauffman, 1969, described from the Miocene and (or) Pliocene Nuwok Formation Member of the Sagavanirktok Formation on the Alaskan North Slope is easily separated by its more rounded outline, smaller and less prosogyrate umbo, and in having a prominent sulcus, although it is reportedly closely related to T. becca cobbani (Kauffman, 1967). Both of these fossil species have narrow hinge fig, narrow, strongly prosogyrate beaks and a deep radial sulcus, all of which excludes them from Wallerconcha.


The sedimentation rate in this region, derived from seismic lines in Grantz et al. (2011) showing the depth of the Quaternary section at this approximate location, is estimated to be about 0.5 m per 1000 years. Measured sedimentation rates upslope of our site on the nearby Mackenzie prodelta by Bringué and Rochon (2012) of 1.43 m/1000 years indicates our estimated rates are reasonable. The sedimentation rate suggests that Wallerconcha sarae has been continuously present here from about 10,300 years to the near present. The age estimate is derived from the interspersed presence of the Wallerconcha sarae specimens from 0.02–5.16 mbsf in our suite of cores, where 5.16 m of sediment corresponds to an accumulation time of 10,320 years. The actual maximum age is likely greater because we have not taken sediment compaction into account, and there is a distinct possibility that Wallerconcha sarae is present below the penetration depth of our core samples.

Although we cannot be certain that Wallerconcha sarae is extinct, we have used associated specimens to determine the potential age of the deposits where it was collected. The planktic foraminiferan Neogloboquadrina pachyderma (Ehrenberg 1861), a species that has been extinct for 1.8 million years, was collected from the base of the same cores as W. sarae at the same depth as the holotype specimen (4.65 mbsf), thus indicating an early Pleistocene age (Wan et al. 2011). A gastropod columella and part of the upper spire of Neptunea (Mollusca: Gastropoda: Buccinidae) was found at the Canning Seafloor Mound (ECS004230, Core 1P1, section 2, 31 cm) and associated with Wallerconcha sarae. Neptunea are predatory snails well represented in the earliest Miocene to Holocene of the northern Pacific and in the late Pliocene to Holocene of the Arctic and northern Atlantic. The presence of Neptunea gives a maximum age for these deposits of latest Miocene or early Pliocene, after the opening of the Bering Strait (Marincovich and Gladenkov 1999; Marincovich et al. 2002).


We thank the officers and crew of the U.S. Coast Guard Cutter Healy for their professionalism in ship handling and, together with members of the HLY1002 scientific party, for assistance with core recovery. In particular, we recognize the efforts of Commanding Officer Captain William (Bill) J. Rall (USCG), Andrew Stevenson (USGS retired), and USGS marine technicians Jenny White and Peter dal Ferro. John Pohlman, Brian Buczkowski (USGS Woods Hole, Massachussetts), and William Schmoker (Polar TREC Arctic Research Consortium) assisted in sampling the cores. John Taylor (NHMUK) alerted us to the possibility that this species represented a new genus. Marianna Terezow (GNS Science, New Zealand) provided photographs of the holotype of Maorithyas marama. Hiroshi Saito (NSMT) loaned us the holotype of Maorithyas hadalis.

In addition, we thank Diego Gabriel Zelaya (Museo de La Plata, La Plata, Argentina), P. Graham Oliver (NMW.Z) John D. Taylor (NHMUK), Lindsey T. Groves (LACMIP), Mary McGann (USGS), Paula Mikkelsen (Paleontological Research Institute), Richard C. Willan (Museum and Art Gallery of the Northern Territory), and Eugene V. Coan (SBMNH) for their helpful comments on the manuscript.

P. Graham Oliver and Anna M. Holmes provided the images of Spinaxinus sentosus. Daniel Geiger provided images of the periostracum of type specimens of Wallerconcha sarae and Maorithyas hadalis.


  • Bernard FR (1972) The genus Thyasira in western Canada (Bivalvia: Lucinacea). Malacologia 11(2): 365–389.
  • Bernard FR (1979) Bivalve mollusks of the western Beaufort Sea. Natural History Museum of Los Angeles County, Contributions in Science 313: 1–80.
  • Bringué M, Rochon A (2012) Late Holocene paleoceanography and climate variability over the Mackenzie Slope (Beaufort Sea, Canadian Arctic). Marine Geology 291–294: 83–96. doi: 10.1016/j.margeo.2011.11.004
  • Coan EV, Valentich-Scott P (2012) Bivalve seashells of tropical west America: Marine bivalves from Baja California to northern Peru. Santa Barbara Museum of Natural History Monographs 6: iii–xv + 1–1258, pls. 1–326.
  • Dall WH (1900) Contributions to the Tertiary fauna of Florida, with especial reference to the silex beds of Tampa and the Pliocene beds of the Caloosahatchie River, including in many cases a complete revision of the generic groups treated of and their American Tertiary species. Part V. Teleodesmacea: Solen to Diplodonta. Wagner Free Institute of Science of Philadelphia, Transactions 3(5): 949–1218, pls. 36–47.
  • Edwards BD, Saint-Ange F, Pohlman J, Higgins J, Mosher DC, Lorenson TD, Hart PE (2011) Sedimentology of cores recovered from the Canada Basin of the Arctic Ocean. Abstract PP33A–1915 presented at 2011 Fall Meeting, AGU, San Francisco, Calif., 5–9 Dec.
  • Ehrenberg CG (1861) Die Tiefgrun–Verhält–nisse des Oceans am Eingange der Davisstrasse bei Island. Monatsberichte der Königlichen Preussische Akademie der Wissenschaften zu Berlin (for 1861): 275–315.
  • Fleming CA (1950) New Zealand Recent Thyasiridae. Transactions of the Royal Society of New Zealand 78(2–3): 251–254.
  • Fujiwara Y, Kato C, Masui N, Fujikura K, Konima S (2001) Dual symbiosis in the cold-seep thyasirid clam Maorithyas hadalis from the hadal zone in the Japan Trench, western Pacfiic. Marine Ecology Progress Series 214: 151–159. doi: 10.3354/meps214151
  • Fujikura K, Kojima S, Tamaki K, Maki Y, Hunt J, Okutani T (1999) The deepest chemosynthesis-based community yet discovered from the hadal zone, 7326 m deep, in the Japan Trench. Marine Ecology Progress Series 190: 17–26. doi: 10.3354/meps190017
  • Gabb WM (1866) Description of the Tertiary invertebrate fossils. Part 1. Geological Survey of California, Palaeontology 2(1): 1–38, pls. 1–13.
  • Grantz A, Hart PE, Childers VA (2011) Geology and tectonic development of the Amerasia and Canada Basins, Arctic Ocean. In: Spencer AM, Gautier D, Stoupakova A, Embry A, Sorensen K (Eds) Arctic Petroleum Geology 35. Geological Society, London Memoirs, 771–799. doi: 10.1016/j.marpetgeo.2011.11.001
  • Grantz A, Hart PE (2012) Petroleum prospectivity of the Canada Basin, Arctic Ocean. Marine and Petroleum Geology 30: 126–143.
  • Hart PE, Pohlman J, Lorenson TD, Edwards BD (2011) Beaufort Sea deep-water gas hydrate: Piston core recovery from a seafloor mound in a region of widespread BSR occurrence. In: Proceeding of the 7th International Conference on Gas Hydrates (ICGH 2011). Edinburgh Scotland, United Kingdom, July 17–21, 2011, 16 pp.
  • Iredale T (1930) More notes on the marine Mollusca of New South Wales. Records of the Australian Museum 17(9): 384–407. doi: 10.3853/j.0067-1975.17.1930.773
  • Jakobsson MR, Macnab M, Mayer L, Anderson R, Edwards M, Hatzky J, Schenke HW, Johnson P (2008) An improved bathymetric portrayal of the Arctic Ocean: implications for ocean modeling and geological, geophysical, and oceanographic analysis. Geophysical Research Letters 34(7). doi: 10.1029/2008GL033520
  • Kauffman EG (1967) Cretaceous Thyasira from the Western Interior of North America. Smithsonian Miscellaneous Collection 152(1), publication 4695, 159 pp.
  • Kauffman EG (1969) Systematics and evolutionary position of a new Tertiary Thyasira (Bivalvia) from Alaska. Journal of Paleontology 43(5): 1099–1110.
  • Krishtofovich LV (1936) Shells of the Thyasira bisecta (Conrad) group from Tertiary deposits on the west coast of Kamchatka. Neftianogo Geologo-Razvedochnogo Instituta, Trudy (A)88: 67 pp.
  • Hryniewicz K, Little CTS, Nakrem HA (2014) Bivalves from the latest Jurassic-earliest Cretaceous hydrocarbon seep carbonates from central Spitsbergen, Svalbard. Zootaxa 3859: 1–66. doi: 10.11646/zootaxa.3859.1.1
  • Lamarck JB (1818) Histoire naturelle des animaux sans vertébres,... 5. Verdière, Deterville & chez l’auteur, Paris, 612 pp.
  • Lorenson TD, Hart PE, Pohlman J, Edwards BD (2011) Sources and Implications of Hydrocarbon Gases from the Deep Beaufort Sea, Alaska. Abstract PP33A–1918 presented at 2011 Fall Meeting, AGU, San Francisco, California, 5–9 Dec.
  • Marincovich LN Jr, Gladenkov AY (1999) Evidence for an early opening of the Bering Strait. Nature 397: 149–151. doi: 10.1038/16446
  • Okutani O, Fujikura K, Kojima S (1999) Two new hadal bivalves of the Family Thyasiridae from the convergent area of the Japan Trench. Venus 58(2): 49–59.
  • Oliver PG (2014) “Tubular gills” Extreme gill modification in the Thyasiroidea with the description of Ochetoctena tomasi gen. et sp. nov. (Bivalvia: Thyasiroidea). Zoosystematics and Evolution 90(2): 121–132. doi: 10.3897/zse.90.8323
  • Oliver PG, Rodrigues CF, Carney R, Duperron S (2013) Spinaxinus (Bivalvia: Thyasiroidea) from sulfide biogenerators in the Gulf of Mexico and hydrothermal vents in the Fiji Back Arc: chemosymbiosis and taxonomy. Scientia Marina 77(4): 663–676. doi: 10.3989/scimar.03848.26B
  • Oliver PG, Holmes AM (2006) New species of Thyasiridae (Bivalvia) from chemosynthetic communities in the Atlantic Ocean. Journal of Conchology 39(2): 175–183. doi: 10.1017/S0025315406013270
  • Oliver PG, Holmes AM (2007a) A new species of Axinus (Bivalvia: Thyasiroidea) from the Baby Bare Seamount, Cascadia Basin, NE Pacific with a description of the anatomy. Journal of Conchology 39(4): 363–375.
  • Oliver PG, Holmes AM (2007b) New species of Thyasiridae (Bivalvia) from chemosynthetic communities in the Atlantic Ocean. Journal of Conchology 39(2): 175–183.
  • Oliver PG, Levin L (2006) A new species of the family Thyasiridae (Mollusca: Bivalvia) from the oxygen minimum zone of the Pakistan margin. Journal of the Marine Biology Association 86: 411–416.
  • Oliver PG, Sellanes J (2005) New species of Thyasiridae from a methane seepage area off Concepción, Chile. Zootaxa 1092: 1–20.
  • Pohlman J, Lorenson TD, Hart PE, Ruppel CD, Joseph C, Torres ME, Edwards BD (2011) Evidence for freshwater discharge at a gas hydrate-bearing seafloor mound on the Beaufort Sea continental slope. Abstract GC41B–0813 presented at 2011 Fall Meeting, AGU, San Francisco, Calif., 5–9 Dec.
  • Roberts HH, Carney RS (1997) Evidence of episodic fluid, gas, and sediment venting on the northern Gulf of Mexico continental slope. Economic Geology 92: 863–879. doi: 10.2113/gsecongeo.92.7-8.863
  • Sibuet M, Olu K (1998) Biogeography, biodiversity and fluid dependence of deep-sea cold-seep communities at active passive margins. Deep-Sea Research II 45: 517–567. doi: 10.1016/S0967-0645(97)00074-X
  • Sowerby J (1821) The mineral conchology of Great Britain; or coloured figures and descriptions of those remains of testaceous animals or shells, which have been preserved at various times and depths in the earth, London (Meredith): 4(55): 9–16, pls. 313–318.
  • Taylor JD, Williams ST, Glover EA (2007) Evolutionary relationships of the bivalve family Thyasiridae (Mollusca: Bivalvia), monophyly and superfamily status. Journal of the Marine Biological Association of the United Kingdom 87(2): 565–574. doi: 10.1017/S0025315407054409
  • Verrill AE (1885) Third catalogue of Mollusca recently added to the fauna of the New England coast and the adjacent parts of the Atlantic, consisting mostly of deep-sea species, with notes on others previously recorded. Transactions of the Connecticut Academy of Arts and Sciences 6: 395–452.
  • Wan E, McGann M, Edwards BD (2011) Preliminary plankic and benthic foraminiferal biostratigraphy of cores from the Canada Basin, western Arctic Ocean. Abstract PP33A–1916. American Geophyscial Union, Fall Meeting 2011, San Francisco, CA, 5–9 December 2011.
  • Yabe H, Nomura S (1925) Notes on the Recent and Tertiary species of Thyasira from Japan. Tohoku [Imperial] University, Science Reports (2 - Geology) 83–95 [1–13], pls. 23 [1], 24 [2].
  • Zelaya DG (2009) The genera Thyasira and Parathyasira in the Magellan region and adjacent Antarctic waters (Bivalvia: Thyasiridae). Malacologia 51(2): 271–290. doi: 10.4002/040.051.0204