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Akademický článek

The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum

Autor: Mustafa Y. Kaya, Guillaume Dupont-Nivet, Joost Frieling, Chiara Fioroni, Alexander Rohrmann, Sevinç Özkan Altıner, Ezgi Vardar, Hakan Tanyaş, Mehmut Mamtimin, Guo Zhaojie

Publikováno v: Communications Earth & Environment, Vol 3, Iss 1, Pp 1-10 (2022)

The Eurasian Epicontinental Sea sequestered 720–1300 Gt of organic carbon during the Palaeocene-Eocene Thermal Maximum, according to a palaeogeographic reconstruction and multi-proxy data from a sedimentary sequence in the Tarim Basin, China.

Externí odkaz: https://doaj.org/article/357c21986bfb4d6f91e12cfd2fadf039

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Deep sea benthic foraminiferal record from the Haymana Basin (Turkey): changes in abundance patterns and diversity across Cretaceous-Paleogene boundary

Autor: Sevinç Özkan-Altıner, Ezgi Vardar

In order to reveal the response of benthic foraminifera to Cretaceous-Paleogene (K/Pg) boundary event, a high-resolution benthic foraminiferal study was carried out from a land-based Haymana section which is biostratigraphically complete, and once lo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d6f025a7657e42871c94d7b506209b7d
https://doi.org/10.5194/egusphere-egu21-15764

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Epicontinental seas as efficient carbon sinks: proto-Paratethys & West Siberian seas during the PETM

Autor: Guo Zhaojie, Ezgi Vardar, Alexander Rohrmann, Birgit Plessen, Joost Frieling, Mustafa Kaya, Sevinç Özkan Altıner, Mehmut Mamtimin, Guillaume Dupont-Nivet, Chiara Fioroni

Removal of carbon on geological timescales is generally assumed to be governed by the relative strength of silicate weathering and organic carbon burial. For past transient warming phases organic carbon burial has been considered as a relevant negati

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e109762784158c82e13f17689add705c
https://hdl.handle.net/11380/1204284

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Paleogene evolution and demise of the proto-Paratethys Sea in Central Asia (Tarim and Tajik basins): Role of intensified tectonic activity at ca. 41 Ma

Autor: Ezgi Vardar, Sevinç Özkan Altıner, Niels Meijer, Natasha Barbolini, Mustafa Kaya, Guillaume Dupont-Nivet, Chiara Fioroni, Marius Stoica, Laurie Bougeois, Pierrick Roperch, Guo Zhaojie, Jovid Aminov, Jean-Noël Proust, Joost Frieling, Mehmut Mamtimin

Publikováno v: Basin Research, 31(3), 461. Wiley-Blackwell
Basin Research
Basin Research, Wiley, 2019, 31 (3), pp.461-486. ⟨10.1111/bre.12330⟩
Basin Research, 31(3), 461-486. Wiley-Blackwell
Basin Research, 2019, 31 (3), pp.461-486. ⟨10.1111/bre.12330⟩

The proto‐Paratethys Sea covered a vast area extending from the Mediterranean Tethys to the Tarim Basin in western China during Cretaceous and early Paleogene. Climate modelling and proxy studies suggest that Asian aridification has been governed b

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f32af80f65533946f23cae4415576d4
https://dspace.library.uu.nl/handle/1874/380324

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