Study on the last deglaciation section of sediment core GeoB6211-2
The North Atlantic Ocean underwent an abrupt temperature increase of 9 °C at high latitudes within a couple of decades during the transition from Heinrich event 1 (H1) to the Bølling warm event, but the mechanism responsible for this warming remains uncertain. Here we address this issue, presenting...
Main Authors: | , , , , , |
---|---|
Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2005
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.779878 https://doi.org/10.1594/PANGAEA.779878 |