Arid
DOI10.3389/feart.2019.00314
Pronounced Northwest African Monsoon Discharge During the Mid- to Late Holocene
Hoepker, Sebastian1,2,3; Wu, Henry C.1; Mueller, Peter1,4; Barusseau, Jean Paul5; Vernet, Robert6; Lucassen, Friedrich2,7; Kasemann, Simone A.2,7; Westphal, Hildegard1,2
通讯作者Hoepker, Sebastian ; Wu, Henry C.
来源期刊FRONTIERS IN EARTH SCIENCE
EISSN2296-6463
出版年2019
卷号7
英文摘要The mid- to late Holocene aridification pattern of NW Africa remains a matter of controversial debate. While many marine climate reconstructions indicate a relatively abrupt aridification at similar to 5.5 ka BP, terrestrial palaeoclimate records rather show a spatially and temporally heterogeneous transition towards the modern arid state. To bridge conflicting evidence, we analysed high-resolution (sub-seasonal) ontogenetic oxygen isotope (delta O-18) records and bulk Sr-87/Sr-86 ratios of bivalve shells and fish otoliths of estuarine-associated species. Samples were excavated from archaeological deposits formed during the mid- to late Holocene in a large palaeo-estuary east of the Banc d'Arguin, Mauritania. The mid-Holocene (similar to 5.2 ka BP) delta O-18 records indicated unrealistically high water temperatures when assuming a modern value for delta O-18(Seawater), suggesting a substantial input of isotopically lighter water to the study area. Respective salinity estimates consistently indicated persistent monsoonal discharge. Moreover, Sr-87/Sr-86 ratios of bivalve shells deviated considerably from the rather stable global seawater composition, further supporting the presence of significant terrestrial runoff between 5.0 and 5.3 ka BP. Altogether, our results support doubts regarding an abrupt termination of the African Humid Period (AHP) in the coastal areas of NW Africa, and show that fully marine conditions were established along the Banc d'Arguin by similar to 3.0 ka BP.
英文关键词African Humid Period Mauritania sclerochronology bivalves fish otoliths archaeology oxygen isotopes Sr- 87 Sr-86
类型Article
语种英语
国家Germany ; New Zealand ; France ; Mauritania
开放获取类型gold, Green Published
收录类别SCI-E
WOS记录号WOS:000502776800001
WOS关键词HUMID PERIOD ; HIGH-RESOLUTION ; MOLLUSK SHELLS ; SALOUM DELTA ; BANC DARGUIN ; CLIMATE ; ISOTOPE ; STRONTIUM ; OXYGEN ; DUST
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
EI主题词2019-11-29
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/311016
作者单位1.Leibniz Ctr Trop Marine Res ZMT GmbH, Bremen, Germany;
2.Univ Bremen, Fac Geosci, Bremen, Germany;
3.Univ Waikato, Fac Sci & Engn, Sch Sci, Environm Res Inst, Hamilton, New Zealand;
4.BDG Berufsverband Deutsch Geowissensch eV, Bonn, Germany;
5.Univ Perpignan Via Domitia, UMR 5110, Ctr Format & Rech Environm Mediterraneens, Perpignan, France;
6.Inst Mauritanien Rech Sci, Nouakchott, Mauritania;
7.Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany
推荐引用方式
GB/T 7714
Hoepker, Sebastian,Wu, Henry C.,Mueller, Peter,et al. Pronounced Northwest African Monsoon Discharge During the Mid- to Late Holocene[J],2019,7.
APA Hoepker, Sebastian.,Wu, Henry C..,Mueller, Peter.,Barusseau, Jean Paul.,Vernet, Robert.,...&Westphal, Hildegard.(2019).Pronounced Northwest African Monsoon Discharge During the Mid- to Late Holocene.FRONTIERS IN EARTH SCIENCE,7.
MLA Hoepker, Sebastian,et al."Pronounced Northwest African Monsoon Discharge During the Mid- to Late Holocene".FRONTIERS IN EARTH SCIENCE 7(2019).
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