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Bivalvia in Ancient Hydrocarbon Seeps

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Ancient Hydrocarbon Seeps

Part of the book series: Topics in Geobiology ((TGBI,volume 53))

Abstract

Bivalves are an important part of the methane seep fauna ever since seeps appeared in the geologic record. The chronostratigraphic ranges of seep-inhabiting chemosymbiotic bivalves show an overall increase in diversity at seeps since the Paleozoic. The most common group at Paleozoic and early Mesozoic seeps are modiomorphids, with a few additional records of solemyids and anomalodesmatans. The most common infaunal chemosymbiotic bivalve taxa at modern seeps, lucinids and thyasirids, appeared at seeps in the Late Jurassic and earliest Cretaceous. They diversified during the Cretaceous synchronous with the peak of the “Mesozoic Marine Revolution” and first occurrences of gastropod predatory drill holes in the shells of seep-inhabiting bivalves, soon after the appearance of these gastropods in the mid-Cretaceous. The two dominant bivalve clades of the modern vent and seep fauna, bathymodiolins and vesicomyids, appeared in the Eocene. Their origin has been linked to a deep-water extinction event at the Paleocene-Eocene Thermal Maximum. However, the fossil record of chemosymbiotic bivalves at seeps during this time interval does not display any extinction. Rather, the mid-Eocene appearance of semi-infaunal and epifaunal bivalves such as bathymodiolins and vesicomyids might be linked to a dramatic rise in seawater sulfate concentrations at this time.

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Notes

  1. 1.

    Institutional Abbreviations in the Figure Captions

    • GZG = Geowissenschaftliches Zentrum, University of Göttingen, Germany

    • JUE = Joetsu University of Education, Japan; collection now at the University Museum of University of Tokyo, Japan

    • PMO = Natural History Museum, University of Oslo, Norway

    • PRI = Paleontological Research Institution, Ithaca, USA

    • UMUT = University Museum of Tokyo University, Japan

    • UOA = University of Auckland, New Zealand

    • USNM = Smithsonian Natural History Museum, Washington DC, USA

    • UWBM = University of Washington, Burke Museum, Seattle, USA

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Acknowledgments

We thank Andrzej Kaim for his invitation to contribute to this chapter. We also thank Simon Schneider and Elizabeth M. Harper for their review and useful comments. This work was partly supported by a Grant-in-aid for Scientific Research from the Japan Society for Promotion of Science (C, 26400500, 2014–2016; C, 17K05691, 2017–2019) to KA and RGJ and a National Science Foundation grant (No. 2014/B/ST10/04886) to KH.

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Authors and Affiliations

  1. Department of Geoscience, Joetsu University of Education, Joetsu, Japan

    Kazutaka Amano

  2. Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, Sweden

    Steffen Kiel

  3. Institute of Paleobiology, Polish Academy of Sciences, Warszawa, Poland

    Krzysztof Hryniewicz

  4. College of Science and Engineering, Kanazawa University, Kanazawa, Japan

    Robert G. Jenkins

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  1. Kazutaka Amano
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Correspondence to Kazutaka Amano .

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  1. Institute of Paleobiology, Polish Academy of Sciences, Warszawa, Poland

    Andrzej Kaim

  2. School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, USA

    J. Kirk Cochran

  3. Department of Invertebrate Paleontology, American Museum of Natural History, New York, NY, USA

    Neil H. Landman

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Amano, K., Kiel, S., Hryniewicz, K., Jenkins, R.G. (2022). Bivalvia in Ancient Hydrocarbon Seeps. In: Kaim, A., Cochran, J.K., Landman, N.H. (eds) Ancient Hydrocarbon Seeps. Topics in Geobiology, vol 53. Springer, Cham. https://doi.org/10.1007/978-3-031-05623-9_10

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