Abstract
Seep deposits in the Upper Cretaceous US Western Interior appear today as prominent geomorphic features in the landscape and are called “tepee buttes.” They are widespread and occur, in general, from the Campanian to early Maastrichtian, persisting for approximately 7 Myr. The presence of methane has been confirmed by isotopic analyses of the seep carbonates, which exhibit values of δ13C as low as −50‰ VPDB. The likely source of the methane was biogenic, produced by the decomposition of sedimentary organic matter, originating from the Pierre Shale and underlying formations. The seeps formed in relatively shallow water ≤100 m deep. Variation in the structure, lithofacies, and fossil composition of the seep deposits may reflect differences in the duration and rate of methane emission. Most seep species reflect the background fauna and are not seep-obligate. In some seeps, authigenic precipitation of carbonates resulted in the development of hard, irregular limestone crusts that provided suitable substrates for animals to settle on and attach to, including stalked articulate crinoids, feather stars, sponges, ophiuroids, asteroids, regular and irregular echinoids, tube worms, crabs, bryozoa, and corals. In turn, these communities attracted a diverse suite of other organisms including gastropods, scaphites, baculites, nautilids, fish, and mosasaurs.
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Acknowledgments
At the American Museum of Natural History, we thank Ana Rashkova, Bushra Hussaini, Mary Conway, Kathleen Sarg, and Marion Savas for accessioning material and assigning AMNH numbers, Mariah Slovacek and Ana Raskhova for collecting fossils in the field and preparing specimens, and Stephen Thurston for photographing specimens and preparing figures. We thank Barbara A. Beasley for arranging permits to collect on the Buffalo Gap National Grassland, South Dakota. We thank Cheryl L. Metz for calling our attention to the maps of the Black Hills produced by N. H. Darton. Many students, colleagues, and family members have helped us collect in the field and interpret the results, and we wish to express our thanks to the ranchers, farmers, and private landowners who granted us permission to collect on their property: Malcolm Bedell, Gale Bishop, Shannon Brophy, Jim and Joyce Grier, William Halligan, Kayla Irizarry, Steve Jorgensen, the late Susan Klofak, Ekaterina Larina, Luke Larson, Tom Linn, Jone Naujokaityte, Dustin Perriguey, Remy Rovelli, James Witts, Adiel Klompmaker, Joshua Slattery, Joshua Laird, Christina Robins, Ben Thuy, Aaron Hunter, Tatsuo Oji, Paul Taylor, Ted Hubbard, Daniel Blake, Mary Haas, Andrzek Kaim, George Philips, Robert Jenkins, and all the doctors who treated us after our field injuries. This research was supported, in part, by the N.D. Newell Fund (AMNH). We are grateful for incisive reviews by William Halligan, Stephen Kiel, Russell Shapiro, and Andrzej Kaim whose comments substantially improved this manuscript.
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Landman, N.H. et al. (2022). Methane Seeps in the Late Cretaceous Western Interior Seaway, USA. 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_15
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