Fine scale sediment structure and geochemical signature between eastern and western North Atlantic during Heinrich events 1 and 2
Heinrich iceberg-rafting events 1 and 2 (H1 and H2) in the Labrador Sea are identified by their typical nepheloid-flow deposit sedimentary structure, high bulk carbonate, increase in iceberg-rafted detritus (IRD), and depletion of delta O-18 in the surface-dwelling foraminifer, Neogloboquadrina pach...
Published in: | Quaternary Science Reviews |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon-elsevier Science Ltd
2012
|
Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00265/37641/36841.pdf https://archimer.ifremer.fr/doc/00265/37641/36842.pdf https://doi.org/10.1016/j.quascirev.2012.04.026 https://archimer.ifremer.fr/doc/00265/37641/ |