Zobrazeno 1 - 10
of 17
pro vyhledávání: '"N. Kafousia"'
Autor:
N. Kafousia, Eleni Kaberi, Aristomenis P. Karageorgis, Maria Triantaphyllou, Eleni Koutsopoulou, Aleka Gogou, Grigoris Rousakis, Vasileios Mavromatis
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Maria Triantaphyllou, N. Kafousia, Stergios D. Zarkogiannis, Iuliana Vasiliev, Marc de Rafélis, Alexandra Gogou, Ioanna Bouloubassi, Fanny Kaczmar, George Kontakiotis, Vasileios Karakitsios, Konstantina Agiadi, Nikolaos Pasadakis, Constantine Parinos, Assimina Antonarakou
Publikováno v:
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2019, 34 (2), pp.182-202. ⟨10.1029/2018PA003438⟩
Paleoceanography and Paleoclimatology, 2019, 34 (2), pp.182-202. ⟨10.1029/2018PA003438⟩
21st EGU General Assembly
21st EGU General Assembly, EGU, Apr 2019, Vienna, Austria
Paleoceanography and Paleoclimatology, American Geophysical Union, 2019, 34 (2), pp.182-202. ⟨10.1029/2018PA003438⟩
Paleoceanography and Paleoclimatology, 2019, 34 (2), pp.182-202. ⟨10.1029/2018PA003438⟩
21st EGU General Assembly
21st EGU General Assembly, EGU, Apr 2019, Vienna, Austria
Summarization: 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) da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85192325aaffe6c3453d49a62aa5ac29
https://hal.archives-ouvertes.fr/hal-02193260/file/2018PA003438.pdf
https://hal.archives-ouvertes.fr/hal-02193260/file/2018PA003438.pdf
Autor:
M. De Rafelis, Assimina Antonarakou, N. Kafousia, George Anastasakis, George Kontakiotis, Hara Drinia, Vasileios Karakitsios, Konstantina Agiadi, P.G. Mortyn
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 459:348-364
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 CO 2 interval in Earth's history, which started after th
Autor:
Assimina Antonarakou, Marco Roveri, Stefano Lugli, Rocco Gennari, Vasileios Karakitsios, Marc de Rafélis, N. Kafousia, Vinicio Manzi, George Kontakiotis, Konstantina Agiadi, Maria Triantaphyllou
Publikováno v:
Basin Research
Basin Research, Wiley, 2016, pp.1-31. ⟨10.1111/bre.12173⟩
Basin Research, 2016, pp.1-31. ⟨10.1111/bre.12173⟩
Basin Research, Wiley, 2016, pp.1-31. ⟨10.1111/bre.12173⟩
Basin Research, 2016, pp.1-31. ⟨10.1111/bre.12173⟩
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
Autor:
Assimina Antonarakou, Konstantina Agiadi, N. Kafousia, Jean-Jacques Cornée, Vasileios Karakitsios, George Kontakiotis, E. Manoutsoglou, Pierre Moissette
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, Springer Verlag, 2017, 106 (3), pp.1147-1159. ⟨10.1007/s00531-016-1355-7⟩
International Journal of Earth Sciences, 2017, 106 (3), pp.1147-1159. ⟨10.1007/s00531-016-1355-7⟩
International Journal of Earth Sciences, Springer Verlag, 2017, 106 (3), pp.1147-1159. ⟨10.1007/s00531-016-1355-7⟩
International Journal of Earth Sciences, 2017, 106 (3), pp.1147-1159. ⟨10.1007/s00531-016-1355-7⟩
Summarization: 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 specie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c5a865b9d7232699910bdeeb96d02978
https://hal.archives-ouvertes.fr/hal-01689792
https://hal.archives-ouvertes.fr/hal-01689792
Autor:
Eoghan P. Reeves, N. Kafousia, Simon H. Bottrell, Paul B. Wignall, Robert J. Newton, Jingeng Sha
Publikováno v:
Geology. 39:7-10
Two records of seawater sulfate isotope composition from the Early Jurassic demonstrate that large isotopic gradients existed between the European epicontinental sea and the open Tethys Ocean. These differences can be explained by the modification of
Publikováno v:
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 47 Αρ. 2 (2013): Διεθνές Συνέδριο "Έρευνα και Εκμετάλλευση Ορυκτών Πόρων"; 825-833
Bulletin of the Geological Society of Greece; Vol. 47 No. 2 (2013): International Congress "Exploration and Exploitation of Mineral Resources"; 825-833
Bulletin of the Geological Society of Greece; Vol. 47 No. 2 (2013): International Congress "Exploration and Exploitation of Mineral Resources"; 825-833
Κατά τη διάρκεια του Κατώτερου Τοάρσιου (~ 183 Ma), έχει καταγραφεί μια παγκό- σμια αναταραχή στον κύκλο του άνθρακα, η οποία έχει σημαδευτεί
Publikováno v:
Paleogeography, Palaeoclimatology, Palaeoecology
Paleogeography, Palaeoclimatology, Palaeoecology, 2014, 393, pp.135--145. ⟨10.1016/j.palaeo.2013.11.013⟩
Paleogeography, Palaeoclimatology, Palaeoecology, 2014, 393, pp.135--145. ⟨10.1016/j.palaeo.2013.11.013⟩
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=doi_dedup___::385e64c8c7075352854833570d750589
https://hal.science/hal-01347029
https://hal.science/hal-01347029
Publikováno v:
Geological Magazine
Geological Magazine, Cambridge University Press (CUP), 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩
Geological Magazine, 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩
Geological Magazine, Cambridge University Press (CUP), 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩
Geological Magazine, 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩
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=doi_dedup___::0d85ae4f5edcc800d9cbfde2ff38b24a
https://hal.archives-ouvertes.fr/hal-00661408
https://hal.archives-ouvertes.fr/hal-00661408
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