气候变化领域集成服务门户(CCPortal): Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130;000 years based on diatoms and with comparison to foraminiferal records

CCPortal

DOI	10.1016/j.palaeo.2019.03.006
	Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130;000 years based on diatoms and with comparison to foraminiferal records
	Hoff U.; Rasmussen T.L.; Meyer H.; Koç N.; Hansen J.
发表日期	2019
ISSN	0031-0182
起始页码	150
结束页码	165
卷号	524
英文摘要	Fossil marine diatom assemblages in a sediment core from the central northern Faroe slope in the Norwegian Sea were used to reconstruct palaeoceanographic changes in the surface water mixed layer from the last ~130,000 years (Marine Isotope Stage (MIS) 6/5 transition to MIS 1 (including the Eemian and Holocene interglacials) and to compare the results with previously published results on planktic foraminifera representing the subsurface conditions of the thermocline. Diatom floras from MIS 5 of the Nordic seas have rarely been studied in detail before and never the entire period from pre-Eemian to present. The composition of diatom species together with maxima in absolute abundance of diatoms, indicate two periods of warmer sea surface temperatures correlating with the Eemian and Holocene interglacials, respectively. The Eemian differs from the Holocene in that the Iceland-Faroe Front never developed, suggesting the cold East Icelandic Current (originating from the East Greenland Current) running north of Iceland was reduced or more mixed with Atlantic water than during the Holocene and that the surface temperature and salinity gradients were weaker. The northern Faroe slope was in the early Weichselian of MIS 5d–5a mainly influenced by weaker inflow of Atlantic water and stronger influence of the East Icelandic Current and by seasonal sea-ice cover. During the later part of the Weichselian (MIS 4–MIS 2) cold conditions prevailed with extensive sea-ice cover except during the warmer interstadials. The diatom floras were more sensitive to climate changes than the planktic foraminifera and indicate longer periods with warm surface conditions, and increased influence of the warm Atlantic surface water from the Faroe Current in MIS 5, suggesting a shallower and much steeper thermocline during the transitional periods compared to today. The diatoms are good indicators for Atlantic water inflow and possible convection in the Nordic seas, not merely reflecting orbital variations in insolation as previously suggested. © 2019
英文关键词	Atlantic water; Eemian; Faroe Islands; Holocene; Marine isotope stages (MIS); Nordic seas
语种	英语
scopus关键词	comparative study; diatom; Eemian; foraminifera; fossil assemblage; historical record; Holocene; interglacial; interstadial; marine ecosystem; marine isotope stage; mixed layer; paleoceanography; planktonic foraminifera; reconstruction; sea surface; sea surface temperature; sediment core; temporal variation; thermocline; Weichselian; Arctic Ocean; Atlantic Ocean; East Greenland Current; East Icelandic Current; Faroe Current; Norwegian Sea; Bacillariophyta; Foraminifera; Nitzschia alba
来源期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/150975
作者单位	CAGE – Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT, The Arctic University of Norway, Tromsø, NO-9037, Norway; Alfred Wegener Institute for Polar and Marine Research, Research Potsdam, Telegrafenberg A45-2, Potsdam, D-14473, Germany; Norwegian Polar Institute, Fram Centre, Hjalmar Johansens gt. 14, Tromsø, NO-9296, Norway; Akvaplan-niva AS, Fram Centre, Hjalmar Johansens gt. 14, Tromsø, NO-9296, Norway
推荐引用方式 GB/T 7714	Hoff U.,Rasmussen T.L.,Meyer H.,等. Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130;000 years based on diatoms and with comparison to foraminiferal records[J],2019,524.
APA	Hoff U.,Rasmussen T.L.,Meyer H.,Koç N.,&Hansen J..(2019).Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130;000 years based on diatoms and with comparison to foraminiferal records.Palaeogeography, Palaeoclimatology, Palaeoecology,524.
MLA	Hoff U.,et al."Palaeoceanographic reconstruction of surface-ocean changes in the southern Norwegian Sea for the last ~130;000 years based on diatoms and with comparison to foraminiferal records".Palaeogeography, Palaeoclimatology, Palaeoecology 524(2019).