This study provides one of the first mechanistic explanations for Last Glacial Maximum deep ocean deoxygenation.
Mar / 18 / 2021
Oxygen
Dissolved neodymium isotopes and Rare Earth Elements combined with oxygen isotopes trace water masses in the Fram Strait
Georgi Laukert and co-workers (2017, see reference below) provide new insights into the sources, distribution and mixing of water masses passing the Fram Strait, the gateway between the Arctic Ocean […]
Feb / 02 / 2017
Oxygen biogeochemistry exerts a strong influence on cobalt cycling
This is an important result of the US GEOTRACES East Pacific Zonal Transect (EPZT) cruise (GP16) discussed by Hawco and his co-workers (2016, see reference below). The distribution of dissolved […]
Jan / 13 / 2017
Tracking the sea ice exported from the Siberian Shelf to the Arctic Ocean
An original method based on the use of the couple salinity – δ18O allows determining the fractions of water that had been removed as ice across the shelf and the […]
Nov / 26 / 2015