Results 111 to 120 of about 1,662,610 (136)
The association between Large Igneous Provinces (LIPs) and mass extinctions and anoxic events is attributed to the radical climatic changes in Earth. Even though the Early Cretaceous Paraná–Etendeka Igneous Province has a comparable erupted volume (>1 ...
Richard E. Ernst, Breno L Waichel
exaly +4 more sources
The Mid-Valanginian Weissert Event as Recorded by Calcareous Nannoplankton in the Vocontian Basin
International audienceThe mid-Valanginian Weissert Event represents one of the most significant paleoceanographic events of the Early Cretaceous and is characterized by a major perturbation of the carbon cycle testified by a positive carbon isotope shift,
Laurent Riquier +2 more
exaly +5 more sources
Benthic foraminifera at Ocean Drilling Program (ODP) Hole 692B were studied to understand variations in oxygen and organic-matter fluxes in bottom waters during the Early Cretaceous.
Elisabetta Erba, Víctor M Giraldo-Gomez
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16 pagesInternational audienceThe Geological Time Scale shows large uncertainties on durations and ages of Berriasian to Albian stages (Early Cretaceous), which impact climate and paleoceanographic reconstructions.
Laurent Riquier +2 more
exaly +5 more sources
Some of the next articles are maybe not open access.
Marine Micropaleontology, 2020
Abstract Strata of Valanginian age (Early Cretaceous, 139.8–132.9 Ma) record a 1.5‰ positive carbon isotope excursion (CIE), the Weissert Event. It coincides with volcanic activity of the Parana-Etendeka large igneous province. Unlike the Mesozoic Oceanic Anoxic Events (OAEs), no organic-rich deposits documenting widespread perturbation of the marine
Jorg Mutterlose, André Bornemann
exaly +2 more sources
Abstract Strata of Valanginian age (Early Cretaceous, 139.8–132.9 Ma) record a 1.5‰ positive carbon isotope excursion (CIE), the Weissert Event. It coincides with volcanic activity of the Parana-Etendeka large igneous province. Unlike the Mesozoic Oceanic Anoxic Events (OAEs), no organic-rich deposits documenting widespread perturbation of the marine
Jorg Mutterlose, André Bornemann
exaly +2 more sources
Arabian Journal of Geosciences, 2021
Within the Valanginian–Hauterivian series of the northern Tethyan margin, two organic-rich laminated black shale intervals corresponding to the Valanginian Weissert and the late Hauterivian Faraoni oceanic anoxic events (W-OAE and F-OAE, respectively) are well documented.
Sabrine Ben Ammar, Mohsen Layeb
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Within the Valanginian–Hauterivian series of the northern Tethyan margin, two organic-rich laminated black shale intervals corresponding to the Valanginian Weissert and the late Hauterivian Faraoni oceanic anoxic events (W-OAE and F-OAE, respectively) are well documented.
Sabrine Ben Ammar, Mohsen Layeb
exaly +2 more sources
Valanginian Weissert Oceanic Anoxic Event
Geology, 2004Biotic changes in nannofossils and radiolarians associated with the Valanginian δ 1 3 C anomaly are documented at Ocean Drilling Program Hole 1149B in the Pacific Ocean: they are coeval and similar to those previously documented in the Tethys, suggesting a global perturbation of marine ecosystems.
Elisabetta Erba +2 more
exaly +3 more sources
Palaeogeography, Palaeoclimatology, Palaeoecology, 2013
Abstract High-resolution gamma-ray measurements performed on five biostratigraphically well-dated reference sections from the Vocontian Basin (south-eastern France) are used to develop a new astrochronology of the Valanginian Stage and its subdivisions (i.e. ammonite and calcareous nannofossil zones and subzones).
Laurent Riquier +2 more
exaly +4 more sources
Abstract High-resolution gamma-ray measurements performed on five biostratigraphically well-dated reference sections from the Vocontian Basin (south-eastern France) are used to develop a new astrochronology of the Valanginian Stage and its subdivisions (i.e. ammonite and calcareous nannofossil zones and subzones).
Laurent Riquier +2 more
exaly +4 more sources
Cretaceous Research, 2010
Abstract An integrated stratigraphic subdivision, on the basis of ammonites, belemnites, calpionellids and stable isotope ratios is proposed for the Lower Cretaceous carbonate succession of the Harskut, Kozoskut Ravine profile (HK-12), (Bakony Mts, Hungary).
József Pálfy +2 more
exaly +2 more sources
Abstract An integrated stratigraphic subdivision, on the basis of ammonites, belemnites, calpionellids and stable isotope ratios is proposed for the Lower Cretaceous carbonate succession of the Harskut, Kozoskut Ravine profile (HK-12), (Bakony Mts, Hungary).
József Pálfy +2 more
exaly +2 more sources

