globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2017.07.004
Scopus记录号: 2-s2.0-85028024703
论文题名:
A 1-Ma record of sea surface temperature and extreme cooling events in the North Atlantic: A perspective from the Iberian Margin
作者: Rodrigues T.; Alonso-García M.; Hodell D.A.; Rufino M.; Naughton F.; Grimalt J.O.; Voelker A.H.L.; Abrantes F.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2017
卷: 172
起始页码: 118
结束页码: 130
语种: 英语
英文关键词: Iberian Margin ; Lipid biomarkers ; Mid-latitudes ; Mid-Pleistocene transition ; Sea Surface Temperature
英文摘要: The Iberian Margin is a sensitive area to track high and low latitude processes, and is a key location to understand major past climatic and oceanographic changes. Here we present new biomarker data from IODP Site U1385 (“Shackleton site”) (1017–336 ka) that, when combined with existing data from Cores MD01-2443/4 (last 335 ka), allows us to assess the evolution of sea surface temperature (SST) and meltwater influx over the last 1 Ma at the Iberian Margin. Interglacial periods throughout the last 1 Ma show SST close to 20 °C, even during the so-called “luke-warm” interglacials that are marked by relatively low atmospheric CO2 concentrations. During glacial periods, extremely cold stadial events are recognized at the Iberian Margin, and are very likely related to meltwater discharges from the European and British-Irish ice sheets into the NE Atlantic, which were transported southwards by the Portugal Current. We subdivided the record into four intervals on the basis of the timing and the magnitude of these extremely cold stadials: 1) from 1017 to ∼900 ka, only minor sporadic freshwater input occurred during deglaciations; 2) from 900 to 675 ka extreme cold events occur as terminal stadial events at the beginning of the deglaciations, which results in abrupt deglacial SST shifts; 3) from 675 to 450 ka only a few, very short-lived events are recorded and seldom is there freshwater input at the Iberian Margin; 4) during the last 450 ka the extreme cold events occurred under full glacial conditions, with particularly severe events during MIS 6 and 8. We propose these mid –glacial events are associated with a strong discharges of European ice sheet (EIS). The fact that these extreme cold events do not coincide with deglaciations questions the role of European ice sheet discharges in triggering deglaciations. © 2017 Elsevier Ltd
资助项目: This study used samples provided by the Integrated Ocean Drilling Program (IODP). This research was supported by the Portuguese Foundation for Science and Technology (FCT) through the CLIMHOL project (PTDC/AAC-CLI/100157/2008), DiatBio project (PTDC/AAG-GLO/3737/2012), and CINAMOW (PTDC/MAR-PRO/3396/2014). We are grateful to M. Padilha, W. Soares and C. Monteiro for laboratory assistance. The editor Henning Bauch and anonymous reviewer are thanked for their thoughtful suggestions. T. Rodrigues acknowledge FCT post-doctoral funding through grants (SFRH/BPD/66025/2009 and SFRH/BPD/108600/2015), and MAG post-doctoral grant SFRH/BPD/96960/2013. We also acknowledge CCMAR funding UID/Multi/04326/2013. This research was also supported by the Natural Environmental Research Council Grant NE/K005804/1 to DH and LS and NE/J017922/1 to DH.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59114
Appears in Collections:过去全球变化的重建

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作者单位: Divisão de Geologia e Georecursos Marinhos, Instituto Português do Mar e da Atmosfera, Rua Alfredo Magalhães Ramalho, 6, Lisboa, Portugal; Centro de Ciências do Mar (CCMAR), Universidade do Algarve, Campus de Gambelas, Faro, Portugal; Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, United Kingdom; Institute of Environmental Assessment and Water Research (IDAEA), CSIC, Jordi Girona, 18, Barcelona, Spain; IFREMER - Centre Atlantique (French Research Institute for Exploitation of the Sea), Département EMH (Ecologie et Modèles pour l'Halieutique), Rue de l'Ile d'Yeu, BP 21105, Cedex 3, Nantes, France

Recommended Citation:
Rodrigues T.,Alonso-García M.,Hodell D.A.,et al. A 1-Ma record of sea surface temperature and extreme cooling events in the North Atlantic: A perspective from the Iberian Margin[J]. Quaternary Science Reviews,2017-01-01,172
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