DOI: 10.1016/j.gloplacha.2015.10.010
论文题名: N zooming into the Mediterranean outflow fossil moat during the 1.2-1.8millionyears period (Early-Pleistocene) - An approach by radiogenic and stable isotopes
作者: Lebreiro S.M. ; Antón L. ; Reguera M.I. ; Fernández M. ; Conde E. ; Barrado A.I. ; Yllera A.
刊名: Global and Planetary Change
ISSN: 0921-8181
出版年: 2015
卷: 135 起始页码: 104
结束页码: 118
语种: 英语
英文关键词: Early-Pleistocene
; Foraminifera
; Gulf Cadiz
; LGM-Holocene
; O-C isotopes
; Obliquity
; Pb-Sr isotopes
Scopus关键词: Climate change
; Glacial geology
; Isotopes
; Lead
; Mixing
; Oceanography
; Early pleistocene
; Foraminifera
; Gulf Cadiz
; Holocenes
; Obliquity
; Sr isotopes
; Strontium
; Foraminifera
英文摘要: The fossil Alvarez Cabral erosive Moatcontains hemipelagite, contourite and turbidite facies where oceanography changes in the Mediterranean outflow are archived over the 1.2-1.8Myr time period. Here we used Pb and Sr radiogenic isotopes to trace water masses and sediment source changes, for the first time in twenty glacial-interglacial (G-I) cycles of the Early-Pleistocene interval, and the last Glacial Maximum through Holocene cycle (including the Younger Dryas and Heinrich Stadial-1). A mixing line of Pb isotopes gives reliable low radiogenic 208Pb/204Pb, 206Pb/204Pb, and 206Pb/207Pb typical of Mediterranean Outflow Water (MOW) in one end-member and the signature of high radiogenic isotopes of Atlantic Waters (AW) towards the second end-member. The 87Sr/86Sr isotopes also display two end-members of the mixing line between eolian transport/dust source (0.71) and fluvial transport/weathering source (0.73) previously proposed in the Gulf of Cadiz. Combination of Pb and Sr radiogenic isotopes with O and C stable isotopes of planktonic and benthic foraminifera, and the response of foraminifera benthos over the Early-Pleistocene interval, reveals a direct link between water masses circulation and shifts in G-I. We found a persistent cyclic pattern of MOW circulation and fluvial deposition during glaciations and AW and aeolian influence during interglaciations. On site U1386B/C, the upper-MOW was less ventilated but productive and with high flux of organic flux matter during glacials, while Atlantic Waters were better ventilated, enriched in O, but less productive during interglacials. We infer that shifts in ocean and atmospheric processes in the Gulf of Cadiz were strongly controlled by Earth's obliquity (41kyr-cycle) and 35°NH insolation during the Early-Pleistocene. We propose a correlation in changes in phase-relationship between precession and obliquity. © 2015 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84954141263&doi=10.1016%2fj.gloplacha.2015.10.010&partnerID=40&md5=9588d96d1fc40cd124573ebf2766e67e
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11459
Appears in Collections: 全球变化的国际研究计划 气候变化与战略
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作者单位: Instituto Geológico y Minero de España (IGME), Calle Ríos Rosas, 23, Madrid, Spain
Recommended Citation:
Lebreiro S.M.,Antón L.,Reguera M.I.,et al. N zooming into the Mediterranean outflow fossil moat during the 1.2-1.8millionyears period (Early-Pleistocene) - An approach by radiogenic and stable isotopes[J]. Global and Planetary Change,2015-01-01,135.