Pollen-based quantitative reconstructions of Holocene regional vegetation cover (plant-functional types and land-cover types) in Europe suitable for climate modelling

被引:156
|
作者
Trondman, A. -K. [1 ]
Gaillard, M. -J. [1 ]
Mazier, F. [2 ]
Sugita, S. [1 ,3 ]
Fyfe, R. [4 ]
Nielsen, A. B. [1 ,5 ,6 ]
Twiddle, C. [7 ]
Barratt, P. [8 ]
Birks, H. J. B. [9 ,10 ]
Bjune, A. E. [11 ,12 ]
Bjorkman, L. [13 ]
Brostrom, A. [6 ,14 ]
Caseldine, C. [15 ]
David, R. [16 ]
Dodson, J. [17 ]
Doerfler, W. [18 ]
Fischer, E. [18 ]
van Geel, B. [19 ]
Giesecke, T. [5 ]
Hultberg, T. [20 ]
Kalnina, L. [21 ]
Kangur, M. [3 ]
van der Knaap, P. [22 ]
Koff, T. [3 ]
Kunes, P. [23 ]
Lageras, P. [14 ]
Latalowa, M. [24 ]
Lechterbeck, J. [25 ]
Leroyer, C. [16 ]
Leydet, M. [26 ]
Lindbladh, M. [20 ]
Marquer, L. [1 ,27 ]
Mitchell, F. J. G. [28 ]
Odgaard, B. V. [29 ]
Peglar, S. M. [9 ,10 ]
Persson, T. [6 ]
Poska, A. [27 ,31 ]
Roesch, M. [25 ]
Seppa, H. [30 ]
Veski, S. [31 ]
Wick, L. [32 ]
机构
[1] Linnaeus Univ, Dept Biol & Environm Sci, SE-39182 Kalmar, Sweden
[2] Toulouse Univ Le Mirail, CNRS GEODE UMR 5602, Toulouse, France
[3] Tallinn Univ, Inst Ecol, EE-10120 Tallinn, Estonia
[4] Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England
[5] Univ Gottingen, Dept Palynol & Climate Dynam, Albrecht von Haller Inst Plant Sci, D-37073 Gottingen, Germany
[6] Lund Univ, Dept Geol, SE-22362 Lund, Sweden
[7] Univ Aberdeen, Sch Geosci, Dept Geog & Environm, Aberdeen AB24 3UF, Scotland
[8] Queens Univ Belfast, Sch Geog, Dept Archaeol & Palaeoecol, Belfast BT9 6AX, Antrim, North Ireland
[9] Univ Bergen, Dept Biol, N-5020 Bergen, Norway
[10] Univ Bergen, Bjerknes Ctr Climate Res, N-5020 Bergen, Norway
[11] Uni Res Climate, N-5007 Bergen, Norway
[12] Bjerknes Ctr Climate Res, N-5007 Bergen, Norway
[13] Viscum Pollenanal & Miljohist, S-57142 Nassjo, Sweden
[14] UV Syd, Swedish Natl Heritage Board, Lund, Sweden
[15] Univ Exeter, Coll Life & Environm Sci, Penryn TR10 9FE, England
[16] Univ Rennes 1, Lab Archeosci, UMR CReAAH 6566, F-35042 Rennes, France
[17] ANSTO, Inst Environm Res, Lucas Heights, NSW 2234, Australia
[18] Univ Kiel, Palynol Lab, Inst Ur & Fruhgeschichte, D-24098 Kiel, Germany
[19] Univ Amsterdam, Dept Paleoecol & Landscape Ecol, Inst Biodivers & Ecosyst Dynam, NL-1098 XH Amsterdam, Netherlands
[20] SLU Swedish Univ Agr Sci, Southern Swedish Forest Res Ctr, SE-23053 Alnarp, Sweden
[21] Univ Latvia, Fac Geog & Earth Sci, Riga, Latvia
[22] Univ Bern, Inst Plant Sci, CH-3013 Bern, Switzerland
[23] Charles Univ Prague, Dept Bot, Fac Sci, Prague 12801 2, Czech Republic
[24] Univ Gdansk, Dept Plant Ecol, Lab Palaeoecol & Archaeobot, PL-80308 Gdansk, Poland
[25] State Off Cultural Heritage Baden Wuerttemberg, Lab Archaobot, Esslingen, Germany
[26] Aix Marseille Univ, IMBE, F-13545 Aix En Provence 04, France
[27] Lund Univ, Dept Phys Geog & Ecosyst Sci, SE-22362 Lund, Sweden
[28] Trinity Coll Dublin, Dept Bot, Dublin 2, Ireland
[29] Aarhus Univ, Dept Geosci, DK-8000 Aarhus C, Denmark
[30] Univ Helsinki, Dept Geosci & Geog, Helsinki, Finland
[31] Tallinn Univ Technol, Inst Geol, EE-19086 Tallinn, Estonia
[32] Univ Basel, Dept Environm Sci, CH-4055 Basel, Switzerland
基金
美国国家科学基金会;
关键词
Europe; Holocene; plant-functional types; pollen data; quantitative past land cover; REVEALS model; SOUTHERN SWEDEN; REVEALS-MODEL; CARBON-CYCLE; SOURCE AREA; ALGORITHM; DATABASE; DYNAMICS; REPRESENTATION; SIMULATIONS; MIDHOLOCENE;
D O I
10.1111/gcb.12737
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
We present quantitative reconstructions of regional vegetation cover in north-western Europe, western Europe north of the Alps, and eastern Europe for five time windows in the Holocene [around 6k, 3k, 0.5k, 0.2k, and 0.05k calendar years before present (bp)] at a 1 degrees x1 degrees spatial scale with the objective of producing vegetation descriptions suitable for climate modelling. The REVEALS model was applied on 636 pollen records from lakes and bogs to reconstruct the past cover of 25 plant taxa grouped into 10 plant-functional types and three land-cover types [evergreen trees, summer-green (deciduous) trees, and open land]. The model corrects for some of the biases in pollen percentages by using pollen productivity estimates and fall speeds of pollen, and by applying simple but robust models of pollen dispersal and deposition. The emerging patterns of tree migration and deforestation between 6k bp and modern time in the REVEALS estimates agree with our general understanding of the vegetation history of Europe based on pollen percentages. However, the degree of anthropogenic deforestation (i.e. cover of cultivated and grazing land) at 3k, 0.5k, and 0.2k bp is significantly higher than deduced from pollen percentages. This is also the case at 6k in some parts of Europe, in particular Britain and Ireland. Furthermore, the relationship between summer-green and evergreen trees, and between individual tree taxa, differs significantly when expressed as pollen percentages or as REVEALS estimates of tree cover. For instance, when Pinus is dominant over Picea as pollen percentages, Picea is dominant over Pinus as REVEALS estimates. These differences play a major role in the reconstruction of European landscapes and for the study of land cover-climate interactions, biodiversity and human resources.
引用
收藏
页码:676 / 697
页数:22
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