Meltwater flux from northern ice-sheets to the mediterranean during MIS 12

Meltwater flux from northern ice-sheets to the mediterranean during MIS 12

Planktonic foraminifer oxygen isotopes through MIS 12 were analysed from Ocean Drilling Program Site 977 in the Alboran Sea. After the correction of the sea surface temperature (SST) effect on the δ18O composition of foraminiferal calcite, the resulting seawater δ18O (δ18Ow) was used to reconstruct...

Full description

Bibliographic Details
Main Authors: Alonso-Garcia, M. (Author), Andersen, N. (Author), Azibeiro, L.A (Author), Cacho, I. (Author), Capotondi, L. (Author), Cortina, A. (Author), Flores, J.-A (Author), González-Lanchas, A. (Author), Grimalt, J.O (Author), Lirer, F. (Author), Martrat, B. (Author), Sierro, F.J (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
Adriatic Sea
Alboran Sea
Calcite
Cordilleran Ice Sheet
Foraminifera
Foraminifers
Fresh Water
Freshwater
Glacial
Glacial geology
Glaciers
Heinrich event
Ice
ice sheet
Ice sheet
Ionian sea
Ionian Sea
Isotopes
marine isotope stage
Marine isotope stage 12
Mediterranean
Mediterranean Sea
meltwater
Meltwater
Millennial climate variabilities
Millennial climate variability
Ocean Drilling Program
Oceanography
Oxygen
oxygen isotope
Oxygen isotopes
Palaeoceanography
sea surface temperature
Surface waters
Water
Online Access:View Fulltext in Publisher

Internet

View Fulltext in Publisher

Similar Items