Matches in UGent Biblio for { <https://biblio.ugent.be/publication/411497#aggregation> ?p ?o. }
Showing items 1 to 47 of
47
with 100 items per page.
- aggregation classification "A1".
- aggregation creator B354401.
- aggregation creator B354402.
- aggregation creator B354403.
- aggregation creator B354404.
- aggregation creator B354405.
- aggregation creator B354406.
- aggregation creator B354407.
- aggregation creator B354408.
- aggregation creator B354409.
- aggregation creator B354410.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation date "2008".
- aggregation format "application/pdf".
- aggregation hasFormat 411497.bibtex.
- aggregation hasFormat 411497.csv.
- aggregation hasFormat 411497.dc.
- aggregation hasFormat 411497.didl.
- aggregation hasFormat 411497.doc.
- aggregation hasFormat 411497.json.
- aggregation hasFormat 411497.mets.
- aggregation hasFormat 411497.mods.
- aggregation hasFormat 411497.rdf.
- aggregation hasFormat 411497.ris.
- aggregation hasFormat 411497.txt.
- aggregation hasFormat 411497.xls.
- aggregation hasFormat 411497.yaml.
- aggregation isPartOf urn:issn:0036-8075.
- aggregation language "eng".
- aggregation rights "I have transferred the copyright for this publication to the publisher".
- aggregation subject "Earth and Environmental Sciences".
- aggregation title "Climate-driven ecosystem succession in the Sahara: the past 6000 years".
- aggregation abstract "Desiccation of the Sahara since the middle Holocene has eradicated all but a few natural archives recording its transition from a "green Sahara" to the present hyperarid desert. Our continuous 6000- year paleoenvironmental reconstruction from northern Chad shows progressive drying of the regional terrestrial ecosystem in response to weakening insolation forcing of the African monsoon and abrupt hydrological change in the local aquatic ecosystem controlled by site- specific thresholds. Strong reductions in tropical trees and then Sahelian grassland cover allowed large- scale dust mobilization from 4300 calendar years before the present ( cal yr B. P.). Today's desert ecosystem and regional wind regime were established around 2700 cal yr B. P. This gradual rather than abrupt termination of the African Humid Period in the eastern Sahara suggests a relatively weak biogeophysical feedback on climate.".
- aggregation authorList BK653194.
- aggregation endPage "768".
- aggregation issue "5877".
- aggregation startPage "765".
- aggregation volume "320".
- aggregation aggregates 4094859.
- aggregation aggregates 4094860.
- aggregation isDescribedBy 411497.
- aggregation similarTo science.1154913.
- aggregation similarTo LU-411497.