Sedimentation rates on the Yermak Plateau during different oxygen isotope stages

Three cores of bottom sediments sampled from the Yermak Plateau are scrutinized. Age model based on AMS 14C dating and oxygen isotope stratigraphy (OIS) is presented for the reference core PS 2837. Hypothetical stratigraphic models for cores PS 2834 and PS 2859 are based on lithostratigraphic analys...

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Bibliographic Details
Main Authors: Levitan, Mikhail A, Musatov, Evgeny E, Burtman, M V
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
151-910C
151-912A
Archive of Ocean Data
ARCOD
ARK-VIII/3
ARK-XIII/2
DRILL
Drilling/drill rig
Elevation of event
Event label
Joides Resolution
KAL
Kasten corer
Latitude of event
Leg151
Longitude of event
North Greenland Sea
Ocean Drilling Program
ODP
Polarstern
PS19/245
PS19 ARCTIC91
PS2212-3
PS2834-5
PS2837-5
PS2859-8
PS44
PS44/062
PS44/065
PS44/091
Sedimentation rate
Yermak Plateau
Greenland
Greenland Sea
North Greenland
Yermak plateau
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.785131
https://doi.org/10.1594/PANGAEA.785131
Description
Summary:Three cores of bottom sediments sampled from the Yermak Plateau are scrutinized. Age model based on AMS 14C dating and oxygen isotope stratigraphy (OIS) is presented for the reference core PS 2837. Hypothetical stratigraphic models for cores PS 2834 and PS 2859 are based on lithostratigraphic analyses. Detailed layer-by-layer descriptions of all studied sections are given based on grain size distribution and contents of CaCO3, Corg, and heavy minerals.

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