Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.gloplacha.2018.10.020 |
Mid-Holocene deepening of the Southeast Pacific oxycline | |
Mollier-Vogel, Elfi1; Martinez, Philippe2; Blanz, Thomas1; Robinson, Rebecca3; Desprat, Stephanie2,4; Etourneau, Johan5; Charlier, Karine2; Schneider, Ralph R.1 | |
通讯作者 | Martinez, Philippe |
来源期刊 | GLOBAL AND PLANETARY CHANGE
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ISSN | 0921-8181 |
EISSN | 1872-6364 |
出版年 | 2019 |
卷号 | 172页码:365-373 |
英文摘要 | This study presents new high resolution sedimentary delta N-15 records from piston cores collected within and outside the present-day eastern south Pacific oxygen minimum zone along a latitudinal transect from 3.5 degrees S to 15 degrees S. Radiocarbon dating of foraminifera and organic matter show that the cores cover the Holocene and the last deglaciation with high sedimentation rate allowing interpretations at millennial to centennial timescale. High delta N-15 values, reaching 10 parts per thousand and large amplitude changes, with a magnitude of similar to 4 parts per thousand, are observed in the southern part of the studied area during the last 18 ka BP. In contrast, the northern Peruvian cores located on the edge of the OMZ show low delta N-15 values varying from 4 to 6 parts per thousand with amplitude of only 1 parts per thousand, during the same time period. delta N-15 values decrease in all the studied cores from the last deglaciation to the early Holocene (17 to 8.5 ka BP) and reach a minimum value during the mid-Holocene. The delta N-15 variations are attributed to microbial N-loss to N-2, e.g. denitrification and/or anammox, and the characteristic N-15-enriched signal that is recorded in the underlying sediments under suboxic to anoxic conditions where denitrifiers thrive. Surprisingly, delta N-15 values from cores located within the OMZ show similar values as the more northern cores located outside the OMZ between 5 and 8.5 ka BP. This minimum is not related to local changes in export production, reconstructed from sedimentary organic carbon, total nitrogen and bromine, but appears to be controlled by changes in the ventilation of the area. The low delta N-15 values recorded between 8.5 and 5 ka BP are well correlated with more arid conditions developed along the Peruvian margin and an increase of the sea surface temperature gradient along the Peruvian margin and between the West and East Pacific along the equator, implying an intensification of the Hadley circulation and climatic conditions similar to La Nina-like state. Consequently, these mid-Holocene conditions led to greater ventilation of subsurface waters that deepened the Peruvian oxycline then revealing similar conditions as observed today in the northern part of the study area. |
英文关键词 | Oxygen minimum zone Peruvian margin Holocene ENSO Nitrogen isotopes |
类型 | Article |
语种 | 英语 |
国家 | Germany ; France ; USA ; Spain |
收录类别 | SCI-E |
WOS记录号 | WOS:000456222800027 |
WOS关键词 | EASTERN TROPICAL PACIFIC ; OXYGEN MINIMUM ZONE ; NUTRIENT UTILIZATION ; UPWELLING SYSTEM ; HOLOCENE CHANGES ; ATMOSPHERIC N2O ; EL-NINO ; PERU ; PRODUCTIVITY ; VARIABILITY |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/216061 |
作者单位 | 1.Christian Albrechts Univ Kiel, Inst Geowissensch, Kiel, Germany; 2.Univ Bordeaux, CNRS, UMR 5805, EPOC, Pessac, France; 3.Univ Rhode Isl, Grad Sch Oceanog, Narrangasett, RI USA; 4.PSL Res Univ, EPHE, Pessac, France; 5.CSIC, Inst Andaluz Ciencias Tierra, Granada, Spain |
推荐引用方式 GB/T 7714 | Mollier-Vogel, Elfi,Martinez, Philippe,Blanz, Thomas,et al. Mid-Holocene deepening of the Southeast Pacific oxycline[J],2019,172:365-373. |
APA | Mollier-Vogel, Elfi.,Martinez, Philippe.,Blanz, Thomas.,Robinson, Rebecca.,Desprat, Stephanie.,...&Schneider, Ralph R..(2019).Mid-Holocene deepening of the Southeast Pacific oxycline.GLOBAL AND PLANETARY CHANGE,172,365-373. |
MLA | Mollier-Vogel, Elfi,et al."Mid-Holocene deepening of the Southeast Pacific oxycline".GLOBAL AND PLANETARY CHANGE 172(2019):365-373. |
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