气候变化领域集成服务门户(CCPortal): Multi-proxy palaeo-data of sediment core GeoB10817-4 from N-Spitsbergen including benthic foraminifera, IRD, stable isotopes, grain sizes and biomarkers

CCPortal

DOI	https://doi.org/10.1594/PANGAEA.882243
	Multi-proxy palaeo-data of sediment core GeoB10817-4 from N-Spitsbergen including benthic foraminifera, IRD, stable isotopes, grain sizes and biomarkers
	Bartels; Martin; Titschack; Jürgen; Fahl; Kirsten; Stein; Ruediger; Seidenkrantz; Marit-Solveig; Hillaire-Marcel; Claude; Hebbeln; Dierk
发布日期	2017-10-26
数据集类型	dataset
英文简介	Atlantic Water (AW) advection plays an important role for climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic Ocean, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection history and document its linkage with local glacier dynamics, as illustrated in the present study of a 275 cm long sedimentary record from Woodfjorden (northern Spitsbergen; water depth: 171 m) spanning the last ~15,500 years. Sedimentological, micropalaeontological and geochemical analyses were used to reconstruct changes in marine environmental conditions, sea-ice cover and glacier activity. Data illustrate a partial breakup of the Svalbard-Barents Sea Ice Sheet from Heinrich Stadial 1 onwards (until ~14.6 ka). During the Bølling-Allerød (~14.6-12.7 ka), AW penetrated as a bottom water mass into the fjord system and contributed significantly to the destabilisation of local glaciers. During the Younger Dryas (~12.7-11.7 ka), it intruded into intermediate waters while evidence for a glacier advance is lacking. A short-term deepening of the halocline occurred at the very end of this interval. During the early Holocene (~11.7-7.8 ka), mild conditions led to glacier retreat, a reduced sea-ice cover and increasing sea surface temperatures, with a brief interruption during the Preboreal Oscillation (~11.1-10.8 ka). Due to a ~6,000-years gap, the mid-Holocene is not recorded in this sediment core. During the late Holocene (~1.8-0.4 ka), a slightly reduced AW inflow and lower sea surface temperatures compared to the early Holocene are reconstructed. Glaciers, which previously retreated to the shallower inner parts of the Woodfjorden system, likely advanced during the late Holocene. In particular, as topographic control in concert with the reduced summer insolation partly decoupled glacier dynamics from AW advection during this recent interval.
空间范围	Median Latitude: 79.800000 * Median Longitude: 14.199950 * South-bound Latitude: 79.800000 * West-bound Longitude: 14.199700 * North-bound Latitude: 79.800000 * East-bound Longitude: 14.200000
时间范围	2006-08-05T00:00:00 - 2006-08-05T22:57:00
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/215291
推荐引用方式 GB/T 7714	Bartels,Martin,Titschack,et al. Multi-proxy palaeo-data of sediment core GeoB10817-4 from N-Spitsbergen including benthic foraminifera, IRD, stable isotopes, grain sizes and biomarkers.2017-10-26.https://doi.org/10.1594/PANGAEA.882243.