TY - JOUR
T1 - A compilation of Western European terrestrial records 60-8kaBP
T2 - Towards an understanding of latitudinal climatic gradients
AU - Data contributors
AU - Moreno, Ana
AU - Svensson, Anders
AU - Brooks, Stephen J.
AU - Connor, Simon
AU - Engels, Stefan
AU - Fletcher, William
AU - Genty, Dominique
AU - Heiri, Oliver
AU - Labuhn, Inga
AU - Perşoiu, Aurel
AU - Peyron, Odile
AU - Sadori, Laura
AU - Valero-Garcés, Blas
AU - Wulf, Sabine
AU - Zanchetta, Giovanni
AU - Allen, Judy R.M.
AU - Ampel, Linda
AU - Blamart, Dominique
AU - Birks, Hillary
AU - Blockley, Simon
AU - Borsato, Andrea
AU - Bos, Hanneke
AU - Brauer, Achim
AU - Combourieu-Nebout, Nathalie
AU - de Beaulieu, Jacques Louis
AU - Drescher-Schneider, Ruth
AU - Drysdale, Russell
AU - Elias, Scott
AU - Frisia, Silvia
AU - Hellstrom, John C.
AU - Ilyashuk, Boris
AU - Joannin, Sebastien
AU - Kühl, Norbert
AU - Larocque-Tobler, Isabelle
AU - Lotter, Andy
AU - Magny, Michel
AU - Matthews, Ian
AU - McDermott, Frank
AU - Millet, Laurent
AU - Morellón, Mario
AU - Neugebauer, Ina
AU - Muñoz-Sobrino, Castor
AU - Naughton, Filipa
AU - Ohlwein, Christian
AU - Roucoux, Katherine
AU - Samartin, Stephanie
AU - Sánchez-Goñi, María Fernanda
AU - Sirocko, Frank
AU - van Asch, Nelleke
AU - van Geel, Bas
PY - 2014/12/15
Y1 - 2014/12/15
N2 - Terrestrial records of past climatic conditions, such as lake sediments and speleothems, provide data of great importance for understanding environmental changes. However, unlike marine and ice core records, terrestrial palaeodata are often not available in databases or in a format that is easily accessible to the non-specialist. As a consequence, many excellent terrestrial records are unknown to the broader palaeoclimate community and are not included in compilations, comparisons, or modelling exercises. Here we present a compilation of Western European terrestrial palaeo-records covering, entirely or partially, the 60-8-ka INTIMATE time period. The compilation contains 56 natural archives, including lake records, speleothems, ice cores, and terrestrial proxies in marine records. The compilation is limited to include records of high temporal resolution and/or records that provide climate proxies or quantitative reconstructions of environmental parameters, such as temperature or precipitation, and that are of relevance and interest to a broader community. We briefly review the different types of terrestrial archives, their respective proxies, their interpretation and their application for palaeoclimatic reconstructions. We also discuss the importance of independent chronologies and the issue of record synchronization. The aim of this exercise is to provide the wider palaeo-community with a consistent compilation of high-quality terrestrial records, to facilitate model-data comparisons, and to identify key areas of interest for future investigations. We use the compilation to investigate Western European latitudinal climate gradients during the deglacial period and, despite of poorly constrained chronologies for the older records, we summarize the main results obtained from NW and SW European terrestrial records before the LGM.
AB - Terrestrial records of past climatic conditions, such as lake sediments and speleothems, provide data of great importance for understanding environmental changes. However, unlike marine and ice core records, terrestrial palaeodata are often not available in databases or in a format that is easily accessible to the non-specialist. As a consequence, many excellent terrestrial records are unknown to the broader palaeoclimate community and are not included in compilations, comparisons, or modelling exercises. Here we present a compilation of Western European terrestrial palaeo-records covering, entirely or partially, the 60-8-ka INTIMATE time period. The compilation contains 56 natural archives, including lake records, speleothems, ice cores, and terrestrial proxies in marine records. The compilation is limited to include records of high temporal resolution and/or records that provide climate proxies or quantitative reconstructions of environmental parameters, such as temperature or precipitation, and that are of relevance and interest to a broader community. We briefly review the different types of terrestrial archives, their respective proxies, their interpretation and their application for palaeoclimatic reconstructions. We also discuss the importance of independent chronologies and the issue of record synchronization. The aim of this exercise is to provide the wider palaeo-community with a consistent compilation of high-quality terrestrial records, to facilitate model-data comparisons, and to identify key areas of interest for future investigations. We use the compilation to investigate Western European latitudinal climate gradients during the deglacial period and, despite of poorly constrained chronologies for the older records, we summarize the main results obtained from NW and SW European terrestrial records before the LGM.
KW - Databases
KW - INTIMATE
KW - Last deglaciation
KW - Terrestrial records
KW - Western Europe
UR - http://www.scopus.com/inward/record.url?scp=84924361085&partnerID=8YFLogxK
U2 - 10.1016/j.quascirev.2014.06.030
DO - 10.1016/j.quascirev.2014.06.030
M3 - Article
AN - SCOPUS:84924361085
SN - 0277-3791
VL - 106
SP - 167
EP - 185
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
ER -