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...

Full description

Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Rashid, H., Saint-ange, Francky, Barber, D. C., Smith, M. E., Devalia, N.
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/