Table 1 - Mercury stable isotope data for Arctic Ocean marine sediments (56 Ma to present) obtained at the University of Michigan by CV-MC-ICPMS (Gleason et al)

Hg stable isotope ratios were obtained by continuous flow cold vapor multi-collector magnetic sector inductively coupled plasma mass spectrometry on ~ 1 gram (dry wt.) sediment from combusted, trapped and purified Hg. Core samples were obtained from Byrd Polar Research Center - Ohio State University...

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Bibliographic Details
Main Authors: Jamie D. Gleason, J.D. Blum, T.C. Moore, L. Polyak, M. Jakobsson, A. Biswas, P.A. Meyers
Format: Dataset
Language:unknown
Published: Arctic Data Center 2013
Subjects:
EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT CHEMISTRY
IN SITU/LABORATORY INSTRUMENTS > SPECTROMETERS/RADIOMETERS > MASS SPECTROMETERS
OTHER
Arctic
Arctic Ocean
Byrd
Byrd Polar Research
Byrd Polar Research Center
Online Access:https://search.dataone.org/view/urn:uuid:bf58a0e0-0706-4472-8051-f75ba2bf6ada
Description
Summary:Hg stable isotope ratios were obtained by continuous flow cold vapor multi-collector magnetic sector inductively coupled plasma mass spectrometry on ~ 1 gram (dry wt.) sediment from combusted, trapped and purified Hg. Core samples were obtained from Byrd Polar Research Center - Ohio State University (Columbus, Ohio), University of Stockholm (Department of Geological Sciences), and IODP-Bremen (Expedition 302).

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