Zobrazeno 1 - 10
of 446
pro vyhledávání: '"J. Levay"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 3, Pp n/a-n/a (2023)
Abstract For over 50 years, cores recovered from ocean basins have generated fossil, lithologic, and chemical archives that have revolutionized fields within the earth sciences. Although scientific ocean drilling (SOD) data are openly available follo
Externí odkaz:
https://doaj.org/article/2d9a24a549384898a072459a33fb1097
Autor:
Heather M. Savage, Srisharan Shreedharan, Åke Fagereng, Julia K. Morgan, Francesca Meneghini, Maomao Wang, David D. McNamara, Laura M. Wallace, Demian M. Saffer, Philip M. Barnes, Katerina E. Petronotis, Leah J. LeVay
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract Quantifying fault damage zones provides a window into stress distribution and rheology around faults. International Ocean Discovery Program (IODP) Expeditions 372/375 drilled an active thrust splay fault within the Hikurangi subduction margi
Externí odkaz:
https://doaj.org/article/c8da92d3ec1a4728b7b4ef24d6f257c8
Autor:
E. J. Screaton, M. E. Torres, B. Dugan, K. U. Heeschen, J. J. Mountjoy, C. Ayres, P. S. Rose, I. A. Pecher, P. M. Barnes, L. J. LeVay
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 6, Pp n/a-n/a (2020)
Abstract Screaton et al. (2019, https://doi.org/10.1029/2019GC008603) examined the role of sedimentation, sea level, and bottom water temperature (BWT) changes due to glaciation as drivers for the downward migration of the base of gas hydrate stabili
Externí odkaz:
https://doaj.org/article/94b49a0fd03045fb988381b97cc921f0
Autor:
A. Sluijs, L. van Roij, G. J. Harrington, S. Schouten, J. A. Sessa, L. J. LeVay, G.-J. Reichart, C. P. Slomp
Publikováno v:
Climate of the Past, Vol 10, Iss 4, Pp 1421-1439 (2014)
The Paleocene–Eocene Thermal Maximum (PETM, ~ 56 Ma) was a ~ 200 kyr episode of global warming, associated with massive injections of 13C-depleted carbon into the ocean–atmosphere system. Although climate change during the PETM is relatively well
Externí odkaz:
https://doaj.org/article/bfcbf45135334b30b29e398f0b9dd1a0
Autor:
Kai Nakajima, Leah J. LeVay, Sidney R. Hemming, Jörg Pross, Rebecca S. Robinson, Ian Hall, Melissa A. Berke, Janna Just, A.M. Franzese, Stefanie Kaboth-Bahr, Andreas Koutsodendris
Publikováno v:
Newsletters on Stratigraphy. 54:159-181
The paleoclimate and ecosystem variability in Africa during the Plio/Pleistocene has received considerable attention due to its potential links to hominid evolution. However, the reconstruction of this variability hinges critically upon highly tempor
Publikováno v:
Paleoceanography and Paleoclimatology, 2022, Vol.37(1), pp.e2021PA004385 [Peer Reviewed Journal]
As a high-nutrient and low-chlorophyll region, the modern Gulf of Alaska (GoA) is strongly impacted by the limitation of iron. Paleostudies along the Alaskan slope have mainly focused on reconstructing environmental conditions over the past 18 ka. Ba
As a high-nutrient and low-chlorophyll region, the modern Gulf of Alaska (GoA) is strongly impacted by the limitation of iron. Paleostudies along the Alaskan slope have mainly focused on reconstruc...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3edff20e11dc27198379df4e282646e0
https://doi.org/10.1002/essoar.10507545.1
https://doi.org/10.1002/essoar.10507545.1
Autor:
Aidan Starr, Leah J. LeVay, Basia Marcks, Melissa A. Berke, Sidney R. Hemming, Isla S. Castañeda, Ian Hall, t. Expedition Scientific Party, A. Cartagena-Sierra, Rebecca S. Robinson
Publikováno v:
Paleoceanography and Paleoclimatology. 36
The meridional variability of the Subtropical Front (STF) in the Southern Hemisphere, linked to expansions or contractions of the Southern Ocean, may have played an important role in global ocean circulation by moderating the magnitude of water excha
Publikováno v:
Earth and Planetary Science Letters. 521:139-149
Early Paleogene neodymium (Nd) isotopic reconstructions of ocean circulation in the Pacific suggest a bipolar mode of overturning circulation characterized by convection of deep-water masses from 70 to at least 40 Ma. This mode is fundamentally diffe