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Hydrocarbon seeps from close to the Jurassic Cretaceous boundary, Svalbard

Hammer, O, Nakrem, HA, Little, CTS, Hryniewicz, K, Sandy, MR, Hurum, JR, Druckenmiller, P, Knutsen, EM and Hoyberget, M (2011) Hydrocarbon seeps from close to the Jurassic Cretaceous boundary, Svalbard. Palaeogeography, Palaeoclimatology, Palaeoecology, 306 (1-2). 15 - 26 . ISSN 0031-0182

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Abstract

Fifteen carbonate bodies, interpreted as having been formed at hydrocarbon seeps, have been found in the Sassenfjorden area of Spitsbergen, Svalbard. The bodies, up to 5 m wide, are found in the siltstones and mudstones of the uppermost Slottsmøya Member, in the Upper Jurassic to lowermost Cretaceous Agardhfjellet Formation. The age of the seeps is close to the Volgian–Ryazanian (Jurassic–Cretaceous) boundary, and the Mjølnir impact event in the Barents Sea. The Sassenfjorden area carbonates show complex and heterogeneous structures typical of hydrocarbon seeps, including zoned (botryoidal) cement textures, fissure-infilling sparite, and breccias. Stable isotope analyses show highly negative δ13C values (down to ca. −43‰ VPDB) in the zoned carbonate cements, consistent with authigenic precipitation in a hydrocarbon-rich environment. Oxygen isotopes indicate secondary hydrothermal activity. The species-rich, well-preserved fauna includes at least 13 species of small to medium sized bivalves, some of which are abundant, as well as rarer rhynchonelliform and lingulid brachiopods, gastropods, echinoderms, sponges, and serpulid and probable vestimentiferan worm tubes. Although several bivalves (solemyids, lucinids, and probably Thyasira and Nucinella) had chemosymbionts, the Sassenfjorden seep fauna contains few, if any, seep obligate taxa, consistent with formation in a relatively shallow-water paleoenvironment. The seeps contain the earliest record of thyasirid bivalves, and a species-rich (six) brachiopod fauna including the first lingulid recorded in a seep environment. Ammonites, belemnites and large wood fragments represent ex situ fossils in the seep carbonate bodies.

Item Type: Article
Academic Units: The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Institute of Geological Sciences (Leeds)
Depositing User: Symplectic Publications
Date Deposited: 25 Jul 2011 15:44
Last Modified: 08 Feb 2013 17:33
Published Version: http://dx.doi.org/10.1016/j.palaeo.2011.03.019
Status: Published
Publisher: Elsevier B.V.
Identification Number: 10.1016/j.palaeo.2011.03.019
URI: http://eprints.whiterose.ac.uk/id/eprint/43152

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