气候变化领域集成服务门户(CCPortal): Pore water chemistry, grain sizes and sediment temperature of 4 sediment cores from submarine permafrost at Mamontov Klyk Cape, Laptev Sea shelf

CCPortal

DOI	https://doi.org/10.1594/PANGAEA.895292
	Pore water chemistry, grain sizes and sediment temperature of 4 sediment cores from submarine permafrost at Mamontov Klyk Cape, Laptev Sea shelf
	Mitzscherling; Julia; Horn; Fabian; Winterfeld; Maria; Mahler; Linda; Kallmeyer; Jens; Overduin; Pier Paul; Winkel; Matthias; Grigoriev; Mikhail N; Wagner; Dirk; Liebner; Susanne
发布日期	2018-10-15
数据集类型	dataset
英文简介	The mobilization of carbon in degrading permafrost is a long-term process and an important feedback upon climate change. Under submarine conditions substantial permafrost warming occurs millennia before permafrost thaws, potentially stimulating microbial communities. How microbial community composition and abundance responded to millennial-scale permafrost warming remains, however, unkown.
空间范围	Median Latitude: 73.640159 * Median Longitude: 117.169868 * South-bound Latitude: 73.605970 * West-bound Longitude: 117.166972 * North-bound Latitude: 73.710028 * East-bound Longitude: 117.177360
时间范围	2005-04-12T00:00:00 - 2005-04-23T00:00:00
语种	英语
国家	国际
学科大类	气候变化
学科子类	气候变化
文献类型	数据集
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/215207
推荐引用方式 GB/T 7714	Mitzscherling,Julia,Horn,et al. Pore water chemistry, grain sizes and sediment temperature of 4 sediment cores from submarine permafrost at Mamontov Klyk Cape, Laptev Sea shelf.2018-10-15.https://doi.org/10.1594/PANGAEA.895292.