Detrital input, productivity fluctuations, and water mass circulation in the westernmost Mediterranean Sea since the Last Glacial Maximum

Detrital input, productivity fluctuations, and water mass circulation in the westernmost Mediterranean Sea since the Last Glacial Maximum

By presenting sea surface temperatures, planktonic oxygen isotope profiles, and bulk geochemical composition of core sediments, we offer a multiparameter reconstruction of Western Mediterranean oceanography from the Last Glacial Maximum until the Middle Holocene (20,000–5000 cal years B. P.). Sedime...

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Bibliographic Details
Main Authors: F. J. Jimenez‐Espejo, F. Martinez‐Ruiz, M. Rogerson, J. M. González‐Donoso, O. E. Romero, D. Linares, T. Sakamoto, D. Gallego‐Torres, J. L. Rueda Ruiz, M. Ortega‐Huertas, J. A. Perez Claros
Format: Article
Language:English
Published: Wiley 2008-11-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
paleoceanography
paleoproductivity
stable isotopes
Alboran front
Holocene/Last Glacial Maximum
ODP 975B
Online Access:https://doi.org/10.1029/2008GC002096

Internet

https://doi.org/10.1029/2008GC002096

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