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  4. Climate and land-use effects on hydrological and vegetation signals during the last three millennia: Evidence from sedimentary leaf waxes in southwestern Morocco
 
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Climate and land-use effects on hydrological and vegetation signals during the last three millennia: Evidence from sedimentary leaf waxes in southwestern Morocco

Journal
Holocene
Journal Volume
31
Journal Issue
5
Pages
699-708
Date Issued
2021
Author(s)
Baqloul A
Schefuß E
Kölling M
Dupont L
JEROEN GROENEVELD  
Zhao X
Reddad H
Bouchaou L
Bouimetarhan I.
DOI
10.1177/0959683620988053
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85099394377&doi=10.1177%2f0959683620988053&partnerID=40&md5=ca6587680ae140cbcbf92c42ddb37722
https://scholars.lib.ntu.edu.tw/handle/123456789/624734
Abstract
The southwest of Morocco is considered to be an area of refuge within the Mediterranean region, hosting the endemic tropical Argan tree. This region is presently subject to severe droughts, desertification and land degradation, and likely facing increased climate variability and socio-economic stress in the future. Here, we use the stable hydrogen and carbon isotope composition (δD and δ13C) of plant-waxes in a high-resolution marine sediment core (GeoB8601-3) collected off Cape Ghir in southwestern Morocco, in combination with published data on pollen and XRF element ratios from the same archive. We aim to reconstruct the hydroclimate and vegetation history during the last 3000 years. Stable carbon isotope compositions of leaf waxes (δ13Cwax) show that natural vegetation in southwestern Morocco consists of C3 plants. Minor variations in δ13Cwax were positively correlated to changes in stable hydrogen isotope compositions of leaf waxes (δDwax) before 700 CE. Changes in rainfall amounts and water use efficiency indicate a clear vegetation response to precipitation changes and thus to climate forcing. After 700 CE, δDwax and δ13Cwax became de-coupled suggesting that the plant wax discharge and their isotope signals were no longer solely controlled by climate; the waxes likely mainly originate from the lowlands and carry an enriched (dry) δD signal but a depleted 13C signature. The depletion of δ13Cwax correlates with the increase of Argan pollen concentration in the record. The period between ~700 and 900 CE coincides with the Arabization of Morocco which had an impact on the demographic composition of the country leading to new agricultural habits and, as a result, on the land-use triggering a higher erosion of lowland material by the Souss River. © The Author(s) 2021.
Subjects
Argan tree; carbon isotopes; climate change; human land-use; Hydrogen isotopes; southwestern Morocco
SDGs

[SDGs]SDG14

Other Subjects
climate change; desertification; drought; hydrogen isotope; hydrometeorology; land use; land use change; marine sediment; precipitation (climatology); rainfall; spatiotemporal analysis; vegetation history; vegetation type; water use efficiency; wax; Cape Ghir; Morocco; Souss-Massa
Type
journal article

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