The Weddell Sea and the associated Filchner–Rønne Ice Shelf constitute key regions for global bottomwater production today. However, little is known about bottom-water production under different climate and icesheet conditions. Therefore, we studied core PS1795, which consists primarily of fine-grained siliciclastic varves that were deposited on contourite ridges in the southeasternWeddell Sea during the Last Glacial Maximum (LGM). We conducted high-resolution X-ray fluorescence (XRF) analysis and grain-size measurements with the RADIUS tool (Seelos and Sirocko, 2005) using thin sections to characterize the two seasonal components of the varves at sub-mm resolution to distinguish the seasonal components of the varves. Bright layers contain...
The thermohaline circulation of the world ocean is partly driven by deep water formation at high-lat...
Arctic and Antarctic polynyas are crucial sites for deep-water formation, which helps sustain global...
Dense shelf water is an essential ingredient to the formation of Antarctic Bottom Water (AABW). It i...
The Weddell Sea and the associated Filchner-Rønne Ice Shelf constitute key regions for global bottom...
Cores from a contourite drift on the continental slope in the NW Weddell Sea, Antarctica, contain up...
Cores from a contourite drift on the continental slope in the NW Weddell Sea, Antarctica, contain up...
Sedimentary processes in the southeastern Weddell Sea are influenced by glacial-interglacial ice-she...
Time-series analyses of satellite images reveal that sea ice extent in the Ross Sea has experienced ...
Abstract: The history of grounded ice-sheet extent on the southern Weddell Sea shelf during the Last...
The geochemical and geochronological fingerprint of rock debris eroded and carried by ice streams ma...
The sediments of 14 box cores and 7 gravity cores, mainly taken directly in front of the Filchner(-R...
Visual counts of ice-rafted debris (IRD), foraminifera, and radiolaria were made for ~1500 samples i...
Arctic and Antarctic polynyas are crucial sites for deep-water formation, which helps sustain global...
For any climate signal to leave an imprint on the Antarctic Bottom Water (AABW) that fills the World...
Sedimentary processes along the Svalbard continental margin are strongly coupled with climate and oc...
The thermohaline circulation of the world ocean is partly driven by deep water formation at high-lat...
Arctic and Antarctic polynyas are crucial sites for deep-water formation, which helps sustain global...
Dense shelf water is an essential ingredient to the formation of Antarctic Bottom Water (AABW). It i...
The Weddell Sea and the associated Filchner-Rønne Ice Shelf constitute key regions for global bottom...
Cores from a contourite drift on the continental slope in the NW Weddell Sea, Antarctica, contain up...
Cores from a contourite drift on the continental slope in the NW Weddell Sea, Antarctica, contain up...
Sedimentary processes in the southeastern Weddell Sea are influenced by glacial-interglacial ice-she...
Time-series analyses of satellite images reveal that sea ice extent in the Ross Sea has experienced ...
Abstract: The history of grounded ice-sheet extent on the southern Weddell Sea shelf during the Last...
The geochemical and geochronological fingerprint of rock debris eroded and carried by ice streams ma...
The sediments of 14 box cores and 7 gravity cores, mainly taken directly in front of the Filchner(-R...
Visual counts of ice-rafted debris (IRD), foraminifera, and radiolaria were made for ~1500 samples i...
Arctic and Antarctic polynyas are crucial sites for deep-water formation, which helps sustain global...
For any climate signal to leave an imprint on the Antarctic Bottom Water (AABW) that fills the World...
Sedimentary processes along the Svalbard continental margin are strongly coupled with climate and oc...
The thermohaline circulation of the world ocean is partly driven by deep water formation at high-lat...
Arctic and Antarctic polynyas are crucial sites for deep-water formation, which helps sustain global...
Dense shelf water is an essential ingredient to the formation of Antarctic Bottom Water (AABW). It i...