Quantification of biotic responses to rapid climatic changes around the Younger Dryas - a synthesis

被引:179
作者
Ammann, B
Birks, HJB
Brooks, SJ
Eicher, U
von Grafenstein, U
Hofmann, W
Lemdahl, G
Schwander, J
Tobolski, K
Wick, L
机构
[1] Univ Bern, Geobot Inst, CH-3013 Bern, Switzerland
[2] Univ Bergen, Inst Bot, N-5007 Bergen, Norway
[3] UCL, Environm Change Res Ctr, London WC1H 0AP, England
[4] Nat Hist Museum, Dept Entomol, London SW7 5BD, England
[5] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland
[6] CEA, CNRS, CFR, F-91198 Gif Sur Yvette, France
[7] Max Planck Inst Limnol, D-24302 Plon, Germany
[8] Univ Vaxjo, Dept Engn & Nat Sci, S-35195 Vaxjo, Sweden
[9] Adam Mickiewicz Univ, Inst Quaternay Res, PL-61701 Poznan, Poland
关键词
biotic response; Late Glacial; quantification; rapid climatic change; time lags;
D O I
10.1016/S0031-0182(00)00092-4
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
To assess the presence or absence of lags in biotic responses to rapid climatic changes, we: (1) assume that the delta(18)O in biogenically precipitated carbonates record global or hemispheric climatic change at the beginning and at the end of the Younger Dryas without any lag at our two study sites of Gerzensee and Leysin, Switzerland; (2) derive a time scale by correlating the delta(18)O record from these two sites with the delta(18)O record of the GRIP ice core; (3) measure delta(18)O records in ostracods and molluscs to check the record in the bulk samples and to detect possible hydrological changes; (4) analyse at Gerzensee and Leysin as well as at two additional sites (that lack carbonates and hence a delta(18)O record) pollen, plant macrofossils, chironomids, beetles and other insects, and Cladocera; (5) estimate our sampling resolution using the GRIP time scale for the isotope stratigraphies and the biostratigraphies; and (6) summarise the major patterns of compositional change in the biostratigraphies by principal component analysis or correspondence analysis. We conclude that, at the major climatic shifts at the beginning and end of the Younger Dryas, hardly any biotic lags occur (within the sampling resolution of 8-30 years) and that upland vegetation responded as fast as aquatic invertebrates. We suggest that the minor climatic changes associated with the Gerzensee and Preboreal oscillations were weakly recorded in the biostratigraphies at the lowland site, but were more distinct at higher altitudes. Individualistic responses of plant and animal species to climatic change may reflect processes in individuals (e.g. productivity and phenology), in populations (e.g. population dynamics), in spatial distributions (e.g. migrations), and in ecosystems (e.g. trophic state). We suggest that biotic responses may be telescoped together into relatively short periods (50 to 150 years), perhaps disrupting functional interactions among species and thus destabilising ecosystems. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:313 / 347
页数:35
相关论文
共 77 条
  • [1] Oxygen-isotope record of Late-Glacial climatic change in western Ireland
    Ahlberg, K
    Almgren, E
    Wright, HE
    Ito, E
    Hobbie, S
    [J]. BOREAS, 1996, 25 (04) : 257 - 267
  • [2] PATTERNS OF VARIATION IN LATE-GLACIAL POLLEN STRATIGRAPHY ALONG A NORTHWEST-SOUTHEAST TRANSECT THROUGH SWITZERLAND - A NUMERICAL-ANALYSIS
    AMMANN, B
    BIRKS, HJB
    DRESCHERSCHNEIDER, R
    JUGGINS, S
    LANG, G
    LOTTER, AF
    [J]. QUATERNARY SCIENCE REVIEWS, 1993, 12 (05) : 277 - 286
  • [3] [Anonymous], [No title captured]
  • [4] Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge
    Bard, E
    Hamelin, B
    Arnold, M
    Montaggioni, L
    Cabioch, G
    Faure, G
    Rougerie, F
    [J]. NATURE, 1996, 382 (6588) : 241 - 244
  • [5] Behre K.-E., 1978, PETERMANN GEOGR MITT, V2, P97
  • [6] Behre K.-E., 1966, EISZEITALTER GEGENWA, V17, P69
  • [7] POST-GLACIAL POPULATION EXPANSION OF FOREST TREES IN NORFOLK, UK
    BENNETT, KD
    [J]. NATURE, 1983, 303 (5913) : 164 - 167
  • [8] Determination of the number of zones in a biostratigraphical sequence
    Bennett, KD
    [J]. NEW PHYTOLOGIST, 1996, 132 (01) : 155 - 170
  • [9] MODELS OF PLANT-POPULATION GROWTH AND ANALOGIES WITH REACTION-KINETICS
    BENNETT, KD
    [J]. REVIEW OF PALAEOBOTANY AND PALYNOLOGY, 1990, 64 (1-4) : 247 - 251
  • [10] LATE WEICHSELIAN ENVIRONMENTAL-CHANGE IN SOUTHERN SWEDEN AND DENMARK
    BERGLUND, BE
    BJORCK, S
    LEMDAHL, G
    BERGSTEN, H
    NORDBERG, K
    KOLSTRUP, E
    [J]. JOURNAL OF QUATERNARY SCIENCE, 1994, 9 (02) : 127 - 132