A high-resolution sea surface temperature (SST) reconstruction of the western Mediterranean was accomplished using two independent, algae-based molecular organic proxies, i.e., the U-37(K) index based on long-chain unsaturated ketones and the novel long-chain diol index (LDI) based on the relative abundances of C-28 and C-30 1,13- and 1,15-diols. Two marine records, from the western and eastern Alboran Sea basin, spanning the last 14 and 20kyr, respectively, were studied. Results from the surface sediments suggest that the two proxies presently reflect seasons with similar SST or simply annual mean SST. Both proxy records reveal the transition from the Last Glacial Maximum to the Holocene in the eastern Alboran Sea with an SST increase of a...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of Am...
A high-resolution sea surface temperature (SST) reconstruction of the western Mediterranean was acco...
A high-resolution sea surface temperature (SST) reconstruction of the western Mediterranean was acco...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
A new high-resolution deglacial and Holocene sea surface temperature (SST) reconstruction is present...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
This study was supported by Grant PID2019-104624RB-I00 funded by MCIN/AEI/ 10.13039/501100011033, Gr...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of Am...
A high-resolution sea surface temperature (SST) reconstruction of the western Mediterranean was acco...
A high-resolution sea surface temperature (SST) reconstruction of the western Mediterranean was acco...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
A new high-resolution deglacial and Holocene sea surface temperature (SST) reconstruction is present...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
Climate conditions in the westernmost Mediterranean (Alboran Sea basin) over the last two millennia ...
This study was supported by Grant PID2019-104624RB-I00 funded by MCIN/AEI/ 10.13039/501100011033, Gr...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Unidad de excelencia María de Maeztu MdM-2015-0552This study presents the reconstructed evolution of...
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of Am...