气候变化领域集成服务门户(CCPortal): Labrador Sea bottom water provenance and REE exchange during the past 35,000 years

CCPortal

DOI	10.1016/j.epsl.2020.116299
	Labrador Sea bottom water provenance and REE exchange during the past 35,000 years
	Blaser P.; Gutjahr M.; Pöppelmeier F.; Frank M.; Kaboth-Bahr S.; Lippold J.
发表日期	2020
ISSN	0012821X
卷号	542
英文摘要	Deep waters of the Labrador Sea (LS) are important contributors to the Atlantic Meridional Overturning Circulation, but their water mass structure has been highly variable and sensitive to climatic changes on different time scales. The LS is also an area of intense exchange of rare earth elements (REE) between seawater and the underlying sediments, which complicates the reconstruction of past deep water provenance based on radiogenic neodymium (Nd) isotopes. Most notably, Northwest Atlantic Bottom Water exchanges Nd with Archaean age Laurentian detritus, resulting in a significant shift to less radiogenic Nd isotope signatures before it enters the North Atlantic to form the deep part of North Atlantic Deep Water. Here we show that the authigenic fractions of LS core top sediments carry Nd isotope signatures intermediate between bottom water and detritus and thus reflect pore waters that incorporate a mixture of both signatures. We furthermore find that detrital imprints on pore waters led to shifts of REE patterns in the authigenic fraction towards detrital signatures in the past during times of enhanced supply of glacially eroded material from Hudson Bay to the LS, as recorded by radiogenic lead isotopes. This allows an estimation of the intensity of past benthic REE exchange inside the LS. We exploit variations in the mid REE enrichment in the authigenic phase to propose a correction to one LS Nd isotope record for detrital imprints originating from pore water exchange. The corrected ϵNd signatures are argued to more accurately reflect those of past bottom waters. This correction results in past LS bottom water signatures of −16 ± 1 during MIS 2 and 3, considerably less radiogenic than today. This implies that no southern sourced waters advanced into the LS during the last 35 ka and instead supports continuous bottom water sourcing from the Nordic Seas. It thus seems likely that LS bottom waters supplied unradiogenic Nd to abyssal Glacial North Atlantic Bottom Water in the Northwest Atlantic, as was previously hypothesized. © 2020 Elsevier B.V.
关键词	boundary exchange Labrador Sea neodymium isotopes paleoceanography rare earth elements weathering
英文关键词	Oceanography; Rare earths; Water; Atlantic meridional overturning circulations; Climatic changes; Different time scale; North Atlantic Deep Water; Northwest Atlantic; Pore water exchange; Radiogenic leads; Water mass structure; Isotopes; bottom water; climate variation; marine isotope stage; meridional circulation; neodymium isotope; overturn; paleoceanography; provenance; rare earth element; reconstruction; Atlantic Ocean; Atlantic Ocean (North); Atlantic Ocean (Northwest); Labrador Sea
语种	英语
来源期刊	Earth and Planetary Science Letters
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/202496
推荐引用方式 GB/T 7714	Blaser P.,Gutjahr M.,Pöppelmeier F.,et al. Labrador Sea bottom water provenance and REE exchange during the past 35,000 years[J],2020,542.
APA	Blaser P.,Gutjahr M.,Pöppelmeier F.,Frank M.,Kaboth-Bahr S.,&Lippold J..(2020).Labrador Sea bottom water provenance and REE exchange during the past 35,000 years.Earth and Planetary Science Letters,542.
MLA	Blaser P.,et al."Labrador Sea bottom water provenance and REE exchange during the past 35,000 years".Earth and Planetary Science Letters 542(2020).