Dissolved organic matter composition in Antarctic streams (Sôya Coast, Lützow-Holm Bay, East Dronning Maud Land, East Antarctica) derived from FT-ICR-MS analyses during JARE58 ...

The sampling campaign was conducted during the austral summer in January 2017 as a part of the 58th Japanese Antarctic Research Expedition. There are several ice-free areas on Sôya Coast with hundreds of lakes and several streams, which were formed during the last 7,000 years under the glacier retre...

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Bibliographic Details
Main Authors: Kida, Morimaru, Fujitake, Nobuhide, Dittmar, Thorsten
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
DOM
NMR
Online Access:https://dx.doi.org/10.1594/pangaea.931814
https://doi.pangaea.de/10.1594/PANGAEA.931814
Description
Summary:The sampling campaign was conducted during the austral summer in January 2017 as a part of the 58th Japanese Antarctic Research Expedition. There are several ice-free areas on Sôya Coast with hundreds of lakes and several streams, which were formed during the last 7,000 years under the glacier retreat and iso-static uplifts that occurred after the Last Glacial Maximum. The Langhovde ice-free area is located ~25 km away from Japan's Syowa Station. The Yukidori and Yatsude Valleys in Langhovde run from the edge of the continental ice sheet to Lutzow-Holm Bay. At each stream of the valleys, water samples were directly collected into 550-mL volume polyethylene terephthalate bottles after rinsing more than three times with the collected water. The collected waters were filtered in a field laboratory within a few hours after sampling. Samples were filtered through pre-combusted (450dc, >3 h) glass-fiber filters (nominal pore size 0.3mm, GF-75, Advantec, Tokyo, Japan) into pre-combusted glass bottles (see ...