气候变化领域集成服务门户(CCPortal): Marine Isotope Stage 11c in Europe: Recent advances in marine-terrestrial correlations and their implications for interglacial stratigraphy

CCPortal

DOI	10.1111/bor.12656
	Marine Isotope Stage 11c in Europe: Recent advances in marine-terrestrial correlations and their implications for interglacial stratigraphy - a review
	Candy, Ian; Oliveira, Dulce; Parkes, Daniel; Sherriff, Jennifer; Thornalley, David
发表日期	2024
ISSN	0300-9483
EISSN	1502-3885
英文摘要	The interglacial known as MIS 11c (c. 426 000-396 000 years ago) receives intensive international interest because of its perceived role as an analogue for the current interglacial and its importance for understanding future climate change. Here we review the current understanding of the stratigraphy of this interglacial in Europe. This study considers (i) the evidence for the environmental history of this interglacial as reconstructed from the varved lake records from northern Europe, (ii) the climate history of MIS 11c as preserved in the long pollen records of southern Europe and (iii) a comparison of both of these with marine records from the North Atlantic. The result of this review is a discussion of the evidence for millennial and centennial scale climate change found in European records of MIS 11c, the patterns of warming that are seen across this interglacial and the discrepancy in aspects of the duration of this interglacial that seems to exist between the marine and terrestrial records of this warm period. A review of the recent advances in the study of MIS 11c in Europe confirms its importance for understanding both the past evolution of the Holocene and the future patterns of long-term climate change. MIS 11c is an interglacial of great importance through its similarities to the current warm period and through characteristics that are relevant to future climate scenarios, i.e. the loss of large parts of the Greenland Ice Sheet. This paper reviews the evidence for the climates of MIS 11c as preserved in palaeoenvironmental archives from across Europe. In particular, we focus on the evidence for abrupt climate change during this interglacial, for which there is abundant evidence on both millennial and centennial timescales. image
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:001204840200001
来源期刊	BOREAS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/309049
作者单位	University of London; Royal Holloway University London; Universidade do Algarve; Instituto Portugues do Mar e da Atmosfera; University of London; University College London; University of London; King's College London
推荐引用方式 GB/T 7714	Candy, Ian,Oliveira, Dulce,Parkes, Daniel,et al. Marine Isotope Stage 11c in Europe: Recent advances in marine-terrestrial correlations and their implications for interglacial stratigraphy - a review[J],2024.
APA	Candy, Ian,Oliveira, Dulce,Parkes, Daniel,Sherriff, Jennifer,&Thornalley, David.(2024).Marine Isotope Stage 11c in Europe: Recent advances in marine-terrestrial correlations and their implications for interglacial stratigraphy - a review.BOREAS.
MLA	Candy, Ian,et al."Marine Isotope Stage 11c in Europe: Recent advances in marine-terrestrial correlations and their implications for interglacial stratigraphy - a review".BOREAS (2024).