Aquatic biota and the detection of climate change: Are there consistent aquatic ecotones?

被引:53
作者
Heegaard, E [1 ]
Lotter, AF
Birks, HJB
机构
[1] Univ Bergen, Bjerknes Ctr Climate Res, Allegaten 55, N-5007 Bergen, Norway
[2] Univ Bergen, Dept Biol, N-5007 Bergen, Norway
[3] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands
[4] UCL, Environm Change Res Ctr, London WC1H 0AP, England
关键词
altitude; beta-diveristy; chironomids; Cladocera; diatoms; multi-proxy studies; palaeoclimatology; reconstructing climate;
D O I
10.1007/s10933-005-3239-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this study, we analyse the cumulative rate of compositional change along an altitudinal gradient in the Swiss Alps for three different groups of aquatic organisms - Cladocera, chironomids, and diatoms. In particular, we are interested in the magnitude of unusually large changes in species composition that allows the detection of critical ecotones for each of these three organism groups. The estimated rate-of-change is the distance in ordination space using principal coordinate analysis based on chord distance and chi-square distance. These analyses highlight the cumulative rate-of-change and the cumulative relative rate-of-change, as the chi-square distance is relative to the total species composition. We found that the major changes in taxonomic composition for the three organism groups and therefore also the major ecotones are just below the modern tree-line (1900-2000 m a.s.l.), which may indirectly be an effect of the tree-line. For diatoms and Cladocera (only chi-square distance) there is also an ecotone at 2055 m a.s.l., which may be a direct or indirect response to climate. Further, the ecotone region below the modern tree-line is much wider for chironomids, with an extension downwards due to a shift in relative abundance patterns. For diatoms there is a stronger rate-of-change above 1650 m a.s.l. when chi-square distance is used. Coupled with the even distribution of diatom richness, this suggests that at higher altitudes the change is more strongly associated with a few species becoming dominant compared to lower elevations. Hence, there are considerable differences among the three organism groups, suggesting that different environmental factors may influence the rates of compositional change within and among groups. This supports the general usefulness of multi-proxy studies, namely the study of several independent groups of organisms to reconstruct past environmental conditions but also points to the importance of careful site selection in such studies.
引用
收藏
页码:507 / 518
页数:12
相关论文
共 88 条
[1]   THE CONFUSION BETWEEN SCALE-DEFINED LEVELS AND CONVENTIONAL LEVELS OF ORGANIZATION IN ECOLOGY [J].
ALLEN, TFH ;
HOEKSTRA, TW .
JOURNAL OF VEGETATION SCIENCE, 1990, 1 (01) :5-12
[2]   Quantitative estimates of recent environmental changes in the Canadian High Arctic inferred from diatoms in lake and pond sediments [J].
Antoniades, D ;
Douglas, MSV ;
Smol, JP .
JOURNAL OF PALEOLIMNOLOGY, 2005, 33 (03) :349-360
[3]  
Arft AM, 1999, ECOL MONOGR, V69, P491, DOI 10.1890/0012-9615(1999)069[0491:ROTPTE]2.0.CO
[4]  
2
[5]   A NEW MODEL FOR THE CONTINUUM CONCEPT [J].
AUSTIN, MP ;
SMITH, TM .
VEGETATIO, 1989, 83 (1-2) :35-47
[6]   Quantitative multiproxy assessment of long-term patterns of Holocene environmental change from a small lake near Abisko, northern Sweden [J].
Bigler, C ;
Larocque, I ;
Peglar, SM ;
Birks, HJB ;
Hall, RI .
HOLOCENE, 2002, 12 (04) :481-496
[7]   The development of the aquatic ecosystem at Krakenes Lake, western Norway, during the late glacial and early Holocene - a synthesis [J].
Birks, HH ;
Battarbee, RW ;
Birks, HJB .
JOURNAL OF PALEOLIMNOLOGY, 2000, 23 (01) :91-114
[8]   Recent environmental change and atmospheric contamination on Svalbard as recorded in lake sediments - synthesis and general conclusions [J].
Birks, HJB ;
Jones, VJ ;
Rose, NL .
JOURNAL OF PALEOLIMNOLOGY, 2004, 31 (04) :531-546
[9]  
Birks HJB, 1981, CLIMATE HIST, P111
[10]  
Blom T, 1998, PROCEEDINGS OF THE SECOND INTERNATIONAL CONFERENCE ON CLIMATE AND WATER, VOLS 1-3, P576