|
|
|
George Kontakiotis, Assimina Antonarakou, Evangelia Besiou, Elisavet Skampa and Maria V. Triantaphyllou
The late Quaternary is a key stratigraphic interval as it encompasses the Late Glacial to Holocene transition, which is characterized by a series of pronounced centennial climate oscillations and subsequent short-term events of paleoceanographic variabil...
ver más
|
|
|
|
|
|
|
Peter K. Bijl,G. Raquel Guerstein,Edgar A. Sanmiguel Jaimes,Appy Sluijs,Silvio Casadio,Victor Valencia,Cecilia R. Amenábar,Alfonso Encinas
Pág. 185 - 218
The tectonic opening of the Tasmanian Gateway and Drake Passage represented crucial geographic requirements for the Cenozoic development of the Antarctic Circumpolar Current (ACC). Particularly the tectonic complexity of Drake Passage has hampered the ex...
ver más
|
|
|
|
|
|
|
Haifeng Wang, Liang Yi, Xiguang Deng and Gaowen He
Global climate and oceanic water masses have undergone profound changes during the middle Pleistocene transition; however, due to a lack of foraminiferal fossils, the nonfossiliferous pelagic deposits were less detected in previous reports. In this work,...
ver más
|
|
|
|
|
|
|
Francisco Serrano
From the study of the planktonic foraminifer assemblages of the sediments of the Ocean Drilling Program (ODP)-Site 975 (Baleares), sea-surface temperature, seasonality and salinity for the Pliocene and Gelasian of the Western Mediterranean were estimated...
ver más
|
|
|
|
|
|
|
Arghya Goswami, Linda Hinnov, Anand Gnanadesikan and Taylor Young
At present, global paleoclimate simulations are prepared with bathtub-like, flat, featureless and steep walled ocean bathymetry, which is neither realistic nor suitable. In this article, we present the first enhanced version of a reconstructed paleobathy...
ver más
|
|
|
|
|
|
|
Eulogio Pardo-Igúzquiza and Francisco J. Rodríguez-Tovar
Many studies have revealed the cyclicity of past ocean/atmosphere dynamics at a wide range of time scales (from decadal to millennial time scales), based on the spectral analysis of time series of climate proxies obtained from deep sea sediment cores. Am...
ver más
|
|
|
|