FN Archimer Export Format
PT J
TI Geochemical methods to infer landscape response to Quaternary climate change and land use in depositional archives: A review
BT 
AF Francke, Alexander
   Holtvoeth, Jens
   Codilean, Alexandru
   Lacey, Jack H.
   Bayon, Germain
   Dosseto, Anthony
AS 1:1,2;2:3;3:1,2,4;4:5;5:6;6:1,2,4;
FF 1:;2:;3:;4:;5:PDG-REM-GM-LGS;6:;
C1 Wollongong Isotope Geochronology Laboratory, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, Australia
   GeoQuEST Research Centre, School of Earth, Atmosphere, and Life Science, University of Wollongong, Wollongong, NSW, Australia
   School of Earth Sciences, University of Bristol, Bristol, United Kingdom
   ARC Centre of Excellence for Australian Biodiversity and Heritage (CABAH), University of Wollongong, Wollongong, NSW, Australia
   National Environmental Isotope Facility, British Geological Survey, Nottingham, United Kingdom
   IFREMER, Marine Geosciences Unit, Brest, France
C2 UNIV WOLLONGONG, AUSTRALIA
   UNIV WOLLONGONG, AUSTRALIA
   UNIV BRISTOL, UK
   UNIV WOLLONGONG, AUSTRALIA
   BRITISH GEOL SURVEY, UK
   IFREMER, FRANCE
SI BREST
SE PDG-REM-GM-LGS
IN WOS Ifremer UPR
   copubli-europe
   copubli-int-hors-europe
IF 12.413
TC 12
UR https://archimer.ifremer.fr/doc/00632/74383/74084.pdf
LA English
DT Article
DE ;Quaternary landscape evolution;Catchment erosion;Terrestrial habitat change;Land use;Fluvial;Lacustrine;Inorganic geochemistry;Organic geochemistry;Radiogenic isotopes;Metal isotopes;Uranium isotopes;Cosmogenic nuclides
AB Understanding and quantifying the processes and geochemical cycles associated with catchment erosion, the development of soils and weathering horizons, and terrestrial habitat change beyond the scales of modern observations remain challenging. Such research, however, has become increasingly important to help predict future landscape change in light of increasing land use and rapid global warming. We herein review organic and inorganic geochemical tools applied to depositional archives to better understand various aspects of landscape evolution on geological time scales. We highlight the potentials and limitations of inorganic geochemical analytical methods, such as major element geochemistry, metal and radiogenic isotopes, and in-situ cosmogenic nuclides, as qualitative, semi-quantitative, and quantitative proxies for the transformation of bedrock material via regolith and soils to sediments. We also show how stable isotope geochemistry applied to lacustrine endogenic carbonates can be used to infer rock-water interactions, vegetation change, and soil development in limestone-rich catchments. Proxies focusing on the silicilastic element of sediment formation, transport and deposition are also ideally combined with organic geochemical proxies for vegetation change and soil organic matter evolution in a catchment to gain a comprehensive picture of the Critical Zone’s evolution over time. Multi-proxy and multidisciplinary research combining organic and inorganic geochemical techniques from several sedimentary archives in the same catchment have high potential to provide comprehensive information on Quaternary landscape evolution and thus improve the robustness of associated forecasting models. 
PY 2020
PD AUG
SO Earth-science Reviews
SN 0012-8252
PU Elsevier BV
VL 207
UT 000556899700011
DI 10.1016/j.earscirev.2020.103218
ID 74383
ER

EF