Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Melody Stein"'
Autor:
Thierry Adatte, Virginie Matera, Dominik Fleitmann, Karl B. Föllmi, Nicolas Fiet, Stéphane Westermann, Melody Stein
Publikováno v:
Geochimica et Cosmochimica Acta. 121:467-486
The early Aptian (125 to 121 Ma) records an episode of severe environmental change including a major perturbation of the carbon cycle, an oceanic anoxic event (OAE 1a, 122.5 Ma), a platform drowning episode and a biocalcification crisis. We propose t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6245fb643cb59ae7aa991cab0f7998b
https://doi.org/10.1016/j.gca.2013.07.023
https://doi.org/10.1016/j.gca.2013.07.023
Autor:
Virginie Matera, Stéphane Westermann, Karl B. Föllmi, Jorge E. Spangenberg, Dominik Fleitmann, Melody Stein, Thierry Adatte
Publikováno v:
Cretaceous Research. 37:209-222
The well-dated section of Cassis-La Bedoule in the South Provencal Basin (southern France) allows for a detailed reconstruction of palaeoenvironmental change during the latest Barremian and Early Aptian. For this study, phosphorus (P) and clay-minera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b848de1769f495b4c30c56362a5d05c
https://doi.org/10.1016/j.cretres.2012.03.021
https://doi.org/10.1016/j.cretres.2012.03.021
Autor:
Dominik Fleitmann, Karl B. Föllmi, Jorge E. Spangenberg, Annie Arnaud-Vanneau, Thierry Adatte, Melody Stein
Publikováno v:
Sedimentology. 59:939-963
A major shift from Urgonian oligotrophic carbonate accumulation to orbitolinid-rich mixed siliciclastic–carbonate deposition is observed near the Barremian–Aptian boundary in many sections both within and outside the shallow-marine Tethyan Realm.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5a80c1f55b124258e7bb2b74c49dda5
https://doi.org/10.1111/j.1365-3091.2011.01286.x
https://doi.org/10.1111/j.1365-3091.2011.01286.x
Autor:
Stéphane Westermann, Zsolt Berner, Dominik Fleitmann, Karl B. Föllmi, Melody Stein, Alexis Godet, Thierry Adatte, Virginie Matera
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 302:396-406
During Oceanic Anoxic Event 1a (OAE 1a, 120 Ma; Li et al., 2008), organic carbon-rich layers were deposited in marine environments under anoxic conditions on a global scale. In this study, palaeoenvironmental conditions leading to this event are char
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9fa7a27ccb175e9f9ea62d02fc26a90
https://doi.org/10.1016/j.palaeo.2011.01.025
https://doi.org/10.1016/j.palaeo.2011.01.025