FN Archimer Export Format
PT J
TI Terrestrial plant microfossils in palaeoenvironmental studies, pollen, microcharcoal and phytolith. Towards a comprehensive understanding of vegetation, fire and climate changes over the past one million years
BT 
AF Daniau, Anne-Laure
   Desprat, Stéphanie
   Aleman, Julie C.
   Bremond, Laurent
   Davis, Basil
   Fletcher, William
   Marlon, Jennifer R.
   Marquer, Laurent
   Montade, Vincent
   Morales-Molino, César
   Naughton, Filipa
   Rius, Damien
   Urrego, Dunia H.
AS 1:1;2:1,2;3:3,5;4:2,5;5:6;6:7;7:8;8:9;9:10;10:11;11:12,13;12:14;13:15;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;
C1 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), Unité Mixte de Recherche (UMR) 5805, Centre National de la Recherche Scientifique (CNRS), Université de Bordeaux, 33615 Pessac, France
   École Pratique des Hautes Études (EPHE), PSL Research University, 75014 Paris, France
   Département de Géographie, Université de Montréal, C.P. 6128, Succ. Centre-Ville, Montréal, Quebec H3C 3J7, Canada
   Laboratoire de Foresterie des Régions tropicales et subtropicales, Gembloux Agro-Bio Tech, Université de Liège, Passage des Déportés 2, 5030 Gembloux, Belgium
   Institut des Sciences de l’Évolution – Montpellier, UMR 5554 CNRS, IRD, Université Montpellier, EPHE, 34000 Montpellier, France
   Institute of Earth Surface Dynamics IDYST, Faculté des Géosciences et l’Environnement, University of Lausanne, Batiment Géopolis, CH-1015 Lausanne, Switzerland
   Department of Geography, School of Environment, Education and Development, University of Manchester, Oxford Road, Manchester M13 9PL, United Kingdom
   School of Forestry & Environmental Studies, Yale University, New Haven, CT 06511, USA
   Research Group for Terrestrial Palaeoclimates, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany
   University of Goettingen, Department of Palynology and Climate Dynamics, Albrecht-von-Haller Institute for Plant Sciences, Wilhelm-Weber-Str. 2a, 37073 Goettingen, Germany
   Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, Altenbergrain 21, 3013 Bern, Switzerland
   Portuguese Sea and Atmosphere Institute (IPMA), Rua Alfredo Magalhães Ramalho 6, 1495-006 Lisboa, Portugal
   Center of Marine Sciences (CCMAR), Algarve University, Campus de Gambelas, 8005-139 Faro, Portugal
   Université de Franche-Comté, Centre National de la Recherche Scientifique (CNRS), Laboratoire Chrono-Environnement, Unité Mixte de Recherche (UMR) 6249, 16, route de Gray, 25030 Besançon cedex, France
   Geography, College of Life and Environmental Sciences, University of Exeter, Amory Building B302, Rennes Drive, Exeter EX4 4RJ, United Kingdom
C2 CNRS, FRANCE
   EPHE, FRANCE
   UNIV MONTREAL, CANADA
   UNIV LIEGE, BELGIUM
   EPHE, FRANCE
   UNIV LAUSANNE, SWITZERLAND
   UNIV MANCHESTER, UK
   UNIV YALE, USA
   MAX PLANCK INST, GERMANY
   UNIV GOTTINGEN, GERMANY
   UNIV BERN, SWITZERLAND
   IPMA, PORTUGAL
   CCMAR, PORTUGAL
   CNRS, FRANCE
   UNIV EXETER, UK
TC 18
UR https://archimer.ifremer.fr/doc/00485/59705/83610.pdf
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
   MD 123 / GEOSCIENCES 1
   MD 134 / PICABIA
   MD 142 / ALIENOR 2
   NAUSICAA-IMAGES 2-MD105
BO Marion Dufresne
DE ;Pollen;Microcharcoal;Phytolith;Terrestrial and marine sedimentary archives;Vegetation;Fire;Middle Pleistocene;Last glacial period;Holocene
AB The Earth has experienced large changes in global and regional climates over the past one million years. Understanding processes and feedbacks that control those past environmental changes is of great interest for better understanding the nature, direction and magnitude of current climate change, its effect on life, and on the physical, biological and chemical processes and ecosystem services important for human well-being. Microfossils from terrestrial plants – pollen, microcharcoal and phytoliths – preserved in terrestrial and marine sedimentary archives are particularly useful tools to document changes in vegetation, fire and land climate. They are well-preserved in a variety of depositional environments and provide quantitative reconstructions of past land cover and climate. Those microfossil data are widely available from public archives, and their spatial coverage includes almost all regions on Earth, including both high and low latitudes and altitudes. Here, we (i) review the laboratory procedures used to extract those microfossils from sediment for microscopic observations and the qualitative and quantitative information they provide, (ii) highlight the importance of regional and global databases for large-scale syntheses of environmental changes, and (iii) review the application of terrestrial plant microfossil records in palaeoclimatology and palaeoecology using key examples from specific regions and past periods. 
PY 2019
PD JUL
SO Revue De Micropaleontologie
SN 0035-1598
PU Elsevier BV
VL 63
UT 000470906300001
BP 1
EP 35
DI 10.1016/j.revmic.2019.02.001
ID 59705
ER

EF