sameAs
New paleocene sepiid coleoids (cephalopoda) from Egypt: evolutionary significance and origin of the sepiid 'rostrum'The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundaryThe Impact of the Latest Danian Event on Planktic Foraminiferal Faunas at ODP Site 1210 (Shatsky Rise, Pacific Ocean)Unsettled puzzle of the Marlboro clays.Early Eocene deep-sea benthic foraminiferal faunas: Recovery from the Paleocene Eocene Thermal Maximum extinction in a greenhouse world.Shelf hypoxia in response to global warming after the Cretaceous-Paleogene boundary impactComment on the paper “Chicxulub impact predates K–T boundary: New evidence from Brazos, Texas” by Keller et al. (2007)Ecological response to collapse of the biological pump following the mass extinction at the Cretaceous–Paleogene boundaryPaleocene–Eocene Thermal Maximum environmental change in the New Jersey Coastal Plain: benthic foraminiferal biotic eventsIntegrated stratigraphy of the Paleocene-Eocene thermal maximum in the New Jersey Coastal Plain: Toward understanding the effects of global warming in a shelf environmentA transient deep-sea circulation switch during Eocene Thermal Maximum 2Persistent environmental change after the Paleocene–Eocene Thermal Maximum in the eastern North AtlanticGeochemical and palaeontological characterization of a new K-Pg Boundary locality from the Northern branch of the Neo-Tethys: Mudurnu – Göynük Basin, NW TurkeyLand–sea coupling of early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcingDifferential response at the seafloor during Palaeocene and Eocene ocean warming events at Walvis Ridge, Atlantic Ocean (ODP Site 1262)Pronounced biotic and environmental change across the latest Danian warming event (LDE) at Shatsky Rise, Pacific Ocean (ODP Site 1210)Taphonomic impact of ultrasonic treatment on foraminifera from a deep-sea carbonate oozeThe demise of the early Eocene greenhouse – Decoupled deep and surface water cooling in the eastern North AtlanticDeep-sea benthic foraminiferal turnovers in the early Eocene: The role of the PETM and ETM2Black shale formation during the Latest Danian Event and the Paleocene?Eocene Thermal Maximum in central Egypt: Two of a kind?Characterization of the Latest Danian Event by means of benthic foraminiferal assemblages along a depth transect at the southern Tethyan margin (Nile Basin, Egypt)Multiple early Eocene benthic foraminiferal assemblage and δ13C fluctuations at DSDP Site 401 (Bay of Biscay — NE Atlantic)Oxygen and carbon isotope fractionation of marine ostracod calcite from the eastern Mediterranean SeaLatest Danian carbon isotope anomaly and associated environmental change in the southern Tethys (Nile Basin, Egypt)An assessment of latest Cretaceous <i>Pycnodonte vesicularis</i> (Lamarck, 1806) shells as records for palaeoseasonality: a multi-proxy investigationAn assessment of latest Cretaceous <i>Pycnodonte vesicularis</i> (Lamarck, 1806) shells as records for palaeoseasonality: A multi-proxy investigationEarly Eocene environmental development in the northern Peri-Tethys (Aktulagay, Kazakhstan) based on benthic foraminiferal assemblages and stable isotopes (O, C)Robust multi-proxy data integration, using late Cretaceous paleotemperature records as a case studyLand–sea coupling of Early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcingOstracode turnover and sea-level changes associated with the Paleocene-Eocene thermal maximumBenthic foraminiferal extinction and repopulation in response to latest Paleocene Tethyan anoxia
P50
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