2013
DOI: 10.1016/j.cretres.2013.08.006
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Upper Campanian–Maastrichtian holostratigraphy of the eastern Danish Basin

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Cited by 81 publications
(89 citation statements)
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“…; Surlyk et al . ). In particular, the study of the expanded Stevns‐1 core has presented a comprehensive holostratigraphical scheme for the Danish Basin, combining lithostratigraphy, micromorphic brachiopod, macrofossil, calcareous nannofossil, dinoflagellate and related palynomorph biostratigraphy, high‐resolution gamma‐ray variations and a high‐resolution carbon‐isotope curve (Surlyk et al .…”
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confidence: 97%
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“…; Surlyk et al . ). In particular, the study of the expanded Stevns‐1 core has presented a comprehensive holostratigraphical scheme for the Danish Basin, combining lithostratigraphy, micromorphic brachiopod, macrofossil, calcareous nannofossil, dinoflagellate and related palynomorph biostratigraphy, high‐resolution gamma‐ray variations and a high‐resolution carbon‐isotope curve (Surlyk et al .…”
mentioning
confidence: 97%
“…In particular, the study of the expanded Stevns‐1 core has presented a comprehensive holostratigraphical scheme for the Danish Basin, combining lithostratigraphy, micromorphic brachiopod, macrofossil, calcareous nannofossil, dinoflagellate and related palynomorph biostratigraphy, high‐resolution gamma‐ray variations and a high‐resolution carbon‐isotope curve (Surlyk et al . ). The Stevns‐1 core has been tied to Site 762C (Indian Ocean) for which an astronomical time‐scale is available for the late Campanian–Maastrichtian interval (Thibault et al .…”
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confidence: 97%
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“…In the uppermost Maastrichtian, this sponge was found in Stevns Klint (Denmark) in the Belemnitella junior-Belemnitella kazimiroviensis Zone (Brünnich and Nielsen 1929;Hansen and Surlyk 2014). The species is also known from other Maastrichtian sections in this part of Europe, as e.g., Germany (Schleswig-Holstein region after Neumann et al 2008), Belgium (Lixhe, province of Liege after Jagt et al 2009) and Denmark (Alaborg, Mons Klint after Brünnich Nielsen 1929, for stratigraphical details see Surlyk et al 2013), however, its precise stratigraphic locations from there are uncertain.…”
Section: ) Of the Zeven Vegen Membermentioning
confidence: 99%
“…The Mesozoic fossil record of Scandinavia and its Arctic territories of Greenland and Svalbard span the dawn of the Triassic some 252 myr ago (Wordie Creek Formation, East Greenland: Nielsen 1935;Bendix-Almgreen 1976;Looy et al 2001;Stemmerik et al 2001;Bjerager et al 2006) through to the terminal Cretaceous -Palaeogene boundary 66 myr ago (Møns Klint Formation, Denmark: Damholt & Surlyk 2012;Surlyk et al 2013;Adolfssen & Ward 2014;Hansen & Surlyk 2014). This interval is marked by the nascence of modern faunal and floral biodiversity, and culminated in one of the most cataclysmic extinction events in Earth history.…”
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confidence: 99%