Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Kafousia, N."'
Autor:
Kontakiotis, G., Karakitsios, V., Mortyn, P.G., Antonarakou, A., Drinia, H., Anastasakis, G., Agiadi, K., Kafousia, N., De Rafelis, M.
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 October 2016 459:348-364
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 January 2014 393:135-145
The Messinian Salinity Crisis (MSC; 5.97–5.33 Ma) is an enigmatic episode of paleoceanographic change, when kilometer-thick evaporite units were deposited in the Mediterranean basin. Here we use geochemical (biomarker and isotope) data to reconstru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::d6df7f61a5945d773c060a58ebeb31c0
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069038
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069038
Environmental change significantly affects the production of fish resources and their dependent societies. The paleontological record offers unique insight into the effects of long-term paleoenvironmental variability on the fish species’ distributi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::06e0760844da1df46d10129746fb8d03
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069469
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069469
This integrated study (field observations, micropalaeontology, magnetostratigraphy, geochemistry, borehole data and seismic profiles) of the Messinian–Zanclean deposits on Zakynthos Island (Ionian Sea) focuses on the sedimentary succession recordin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::38ed4a6acdf0babb683bf9a778c1354b
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069471
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069471
One of the most enigmatic features of long-term Cenozoic climatic evolution, with some analog potential for present/future global climate change, is the last sustained warm and high-atmospheric CO2 interval in Earth's history, which started after the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::a59eb6a852c119edf73cd8ce6794d1f8
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3009594
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3009594
Publikováno v:
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 43 Αρ. 2 (2010): 12o Διεθνές Συνέδριο της Ελληνικής Γεωλογικής Εταιρίας; 627-633
Bulletin of the Geological Society of Greece; Vol. 43 No. 2 (2010): 12th International Conference of the G.S.G.; 627-633
Bulletin of the Geological Society of Greece; Vol. 43 No. 2 (2010): 12th International Conference of the G.S.G.; 627-633
The Early Toarcian Oceanic Anoxic Event (ca 183 Ma) coincides with high palaeotemperatures, regional anoxia to euxinia, marine transgression, mass extinction and high rates of organic-carbon burial in a global context. Most of the detailed studies of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25118b4763efd906449881187e24fc7b
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/11225
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/11225
Publikováno v:
Psicologia em Estudo
Psicologia em Estudo, Universidade Estadual de Campinas, Departamento de Política Científica e Tecnológica, Instituto de Geociências, 2014, 387 (6169), ⟨10.1016/j.palaeo.2013.11.013⟩
Psicologia em Estudo, 2014, 387 (6169), ⟨10.1016/j.palaeo.2013.11.013⟩
Psicologia em Estudo, Universidade Estadual de Campinas, Departamento de Política Científica e Tecnológica, Instituto de Geociências, 2014, 387 (6169), ⟨10.1016/j.palaeo.2013.11.013⟩
Psicologia em Estudo, 2014, 387 (6169), ⟨10.1016/j.palaeo.2013.11.013⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3d7bf6af76208dd0fa3c85db3e6fb5ac
https://hal.archives-ouvertes.fr/hal-01366995
https://hal.archives-ouvertes.fr/hal-01366995
The Early Jurassic was characterized by a global disturbance of the carbon cycle known as the Toarcian Oceanic Anoxic Event (T-OAE). This event is recorded worldwide by a negative excursion in marine and terrestrial carbon-isotope ratios, typically i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::84eeced66fb9be2ee2b7b5375e62b549
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3009870
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3009870
The Early Toarcian (Early Jurassic, c. 183 Ma) was characterized by an Oceanic Anoxic Event (T-OAE), primarily identified by the presence of globally distributed approximately coeval black organic-rich shales. This event corresponded with relatively
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::0ee34faa2623d1a7c8fd418989876422
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070769
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070769