Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2019.109245 |
The antiquity of the Sahara Desert: New evidence from the mineralogy and geochemistry of Pliocene paleosols on the Canary Islands, Spain | |
Muhs, Daniel R.1; Meco, Joaquin2; Budahn, James R.1; Skipp, Gary L.1; Betancort, Juan F.2; Lomoschitz, Alejandro3 | |
通讯作者 | Muhs, Daniel R. |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2019 |
卷号 | 533 |
英文摘要 | The Sahara is the largest warm desert in the world, but its age has been controversial, with estimates ranging from Miocene to Holocene. Mineralogical and geochemical data show that paleosols of Pliocene to mid Pleistocene age on Fuerteventura and Gran Canaria in the Canary Islands have developed in part from inputs of dust from Africa. These paleosols contain quartz and mica, minerals that are abundant in African dust but are rare in the basaltic rocks that dominate the Canary Islands. Trace elements with minimal mobility, Sc, Cr, Hf, Th, and Ta as well as the rare earth elements, show that paleosols have compositions that are intermediate between those of local rocks and African-derived dust. Thus, results reported here and in a recently published study by others indicate that 9 paleosols record delivery of African dust to the Canary Islands between similar to 4.8-2.8 Ma, similar to 3.0-2.9 Ma, similar to 2.3-1.46 Ma, and similar to 0.4 Ma. A long-term paleosol record of African dust input agrees with deepsea records off the coast of western Africa that imply increased dust fluxes to the eastern Atlantic Ocean at similar to 4.6 Ma. It is concluded that the Sahara Desert has been in existence as an arid-region dust source, at least intermittently, for much of the Pliocene and continuing into the Pleistocene. |
英文关键词 | Paleoclimate Aridity African dust Clay minerals Trace elements |
类型 | Article |
语种 | 英语 |
国家 | USA ; Spain |
开放获取类型 | Green Published, Bronze |
收录类别 | SCI-E |
WOS记录号 | WOS:000487174100017 |
WOS关键词 | RARE-EARTH-ELEMENTS ; SEA-LEVEL HISTORY ; GRAN-CANARIA ; NORTH-ATLANTIC ; CONTACT AUREOLE ; PARTICLE-SIZE ; DUST ; FUERTEVENTURA ; CLIMATE ; EVOLUTION |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
EI主题词 | 2019-11-01 |
来源机构 | United States Geological Survey |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/310711 |
作者单位 | 1.US Geol Survey, Fed Ctr, MS 980,Box 25046, Denver, CO 80225 USA; 2.Univ Las Palmas Gran Canaria, Dept Biol, Las Palmas Gran Canaria 35017, Canary Islands, Spain; 3.Univ Las Palmas Gran Canaria, Inst Oceanog & Cambio Global, CSIC, Unidad Asociada IDi,IOCAG, Las Palmas Gran Canaria 35017, Canary Islands, Spain |
推荐引用方式 GB/T 7714 | Muhs, Daniel R.,Meco, Joaquin,Budahn, James R.,et al. The antiquity of the Sahara Desert: New evidence from the mineralogy and geochemistry of Pliocene paleosols on the Canary Islands, Spain[J]. United States Geological Survey,2019,533. |
APA | Muhs, Daniel R.,Meco, Joaquin,Budahn, James R.,Skipp, Gary L.,Betancort, Juan F.,&Lomoschitz, Alejandro.(2019).The antiquity of the Sahara Desert: New evidence from the mineralogy and geochemistry of Pliocene paleosols on the Canary Islands, Spain.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,533. |
MLA | Muhs, Daniel R.,et al."The antiquity of the Sahara Desert: New evidence from the mineralogy and geochemistry of Pliocene paleosols on the Canary Islands, Spain".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 533(2019). |
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