FN Archimer Export Format
PT J
TI Controls on Holocene denudation rates in mountainous environments under Mediterranean climate
BT 
AF MOLLIEX, S.
   JOUET, Gwenael
   FRESLON, Nicolas
   BOURLES, D. L.
   AUTHEMAYOU, C.
   MOREAU, Julien
   RABINEAU, Marina
AS 1:1,2;2:1;3:1,3;4:3;5:2;6:1,3;7:2;
FF 1:;2:PDG-REM-GM-LGS;3:PDG-REM-GM-LCG;4:;5:;6:PDG-REM-GM-LES;7:;
C1 IFREMER, Dept Geosci Marines, F-29280 Plouzane, France.
   Univ Bretagne Occidentale, Inst Univ Europeen Mer, UMR CNRS 6538, Lab Domaines Ocean, F-29280 Plouzane, France.
   Aix Marseille Univ, Coll France, CNRS, CEREGE,UM34,IRD, BP80, F-13545 Aix En Provence 4, France.
C2 IFREMER, FRANCE
   UBO, FRANCE
   UNIV AIX MARSEILLE, FRANCE
SI BREST
SE PDG-REM-GM-LGS
   PDG-REM-GM-LCG
   PDG-REM-GM-LES
UM LGO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 3.722
TC 6
UR https://archimer.ifremer.fr/doc/00380/49082/49655.pdf
LA English
DT Article
DE ;Be-10-derived denudation rates;Schmidt Hammer;Quaternary;quantitative geomorphology;weathering
AB The Mediterranean domain is characterized by a specific climate resulting from the close interplay between atmospheric and marine processes and strongly differentiated regional topographies. Corsica Island, a mountainous area located in the western part of the Mediterranean Sea is particularly suitable to quantify regional denudation rates in the framework of a source-to-sink approach. Indeed, fluvial sedimentation in East-Corsica margin is almost exclusively limited to its alluvial plain and offshore domain and its basement is mainly constituted of quartz-rich crystalline rocks allowing cosmogenic nuclide Be-10 measurements. In this paper, Holocene denudation rates of catchments from the eastern part of the island of Corsica are quantified relying on in situ produced Be-10 concentrations in stream sediments and interpreted in an approach including quantitative geomorphology, rock strength measurement (with a Schmidt Hammer) and vegetation cover distribution. Calculated denudation rates range from 15 to 95 mm ka(-1). When compared with rates from similar geomorphic domains experiencing a different climate setting, such as the foreland of the northern European Alps, they appear quite low and temporally stable. At the first order, they better correlate with rock strength and vegetation cover than with morphometric indexes. Spatial distribution of the vegetation is controlled by morpho-climatic parameters including sun exposure and the direction of the main wet wind, so-called Libecciu'. This distribution, as well as the basement rock strength seems to play a significant role in the denudation distribution. We thus suggest that the landscape reached a geomorphic steady-state due to the specific Mediterranean climate and that Holocene denudation rates are mainly sustained by weathering processes, through the amount of regolith formation, rather than being transport-limited. Al/K measurements used as a proxy to infer present-day catchment-wide chemical weathering patterns might support this assumption. 
PY 2017
PD FEB
SO Earth Surface Processes And Landforms
SN 0197-9337
PU Wiley
VL 42
IS 2
UT 000394689000003
BP 272
EP 289
DI 10.1002/esp.3987
ID 49082
ER

EF