TEMPORAL SCALE, PHYTOPLANKTON ECOLOGY AND PALEOLIMNOLOGY

被引:21
作者
ANDERSON, NJ
机构
[1] Geobotany Division, Danish Geological Survey, Copenhagen, Nevada, DK-2400
关键词
D O I
10.1111/j.1365-2427.1995.tb00895.x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
1. Scales of temporal analysis in limnology generally cover diel through to interannual changes, with occasional longer studies with up to 50 years continuous sampling data. Lakes, however, have been changing over much longer time periods than this, as is apparent from palaeolimnological studies. Temporal scales are, however, largely relative, with an individual's perspective controlling what is deemed short or long term. 2. Phytoplankton populations are variable over a variety of timescales, and the sediment record can readily record these changes from interannual through to 10(3)-year timescales. Because of anthropogenic influences, such as acidification and eutrophication, phytoplankton communities probably have been altered dramatically in many lakes, often before routine sampling began. Records of changing phytoplankton populations at timescales relevant to limnologists can be derived from, for example, varved sediments and used to address specific problems, such as the degree of long-term interannual variability and timescales of sexual reproduction. 3. Palaeolimnologists tend to interpret changes in sediment assemblages in terms of ecological and physiological processes which are relevant at scales that may not be resolvable in lake sediments. There is a clear need for sediment records to be interpreted in terms of the processes which operate at timescales that match the resolution of that sediment sequence. 4. Increasingly fine sampling resolutions are being attempted by palaeolimnologists, often without consideration of the reasons for such an approach or to the repeatability of the results. The increased variability associated with high-resolution sampling can make it difficult to separate noise from the ecological signal. There is a clear need for replication. 5. The necessary temporal resolution is defined by the aim of any given palaeolimnological study. If the main emphasis of a study is, for example, establishing background phosphorus concentrations, a coarser sampling resolution is probably acceptable than that required for many 'ecological' studies.
引用
收藏
页码:367 / 378
页数:12
相关论文
共 67 条
[1]  
Anderson N.J., 1994, P233
[2]   SPATIAL HETEROGENEITY OF DIATOM STRATIGRAPHY IN VARVED AND NON-VARVED SEDIMENTS OF A SMALL, BOREAL-FOREST LAKE [J].
ANDERSON, NJ ;
KORSMAN, T ;
RENBERG, I .
AQUATIC SCIENCES, 1994, 56 (01) :40-58
[3]   USING THE PAST TO PREDICT THE FUTURE - LAKE-SEDIMENTS AND THE MODELING OF LIMNOLOGICAL DISTURBANCE [J].
ANDERSON, NJ .
ECOLOGICAL MODELLING, 1995, 78 (1-2) :149-172
[4]  
ANDERSON NJ, 1993, TRENDS ECOL EVOL, V8, P356
[5]  
[Anonymous], 1984, ECOLOGY FRESHWATER P
[6]  
BATTARBEE RW, 1991, QUATERNARY LANDSCAPE, P129
[7]  
BATTARBEE RW, 1984, PHIL T R SOC LONDO B, V305, P415
[8]   QUATERNARY PALEOECOLOGY AND VEGETATION SCIENCE - CURRENT CONTRIBUTIONS AND POSSIBLE FUTURE-DEVELOPMENTS [J].
BIRKS, HJB .
REVIEW OF PALAEOBOTANY AND PALYNOLOGY, 1993, 79 (1-2) :153-177
[9]  
Carpenter S.R., 1993, TROPHIC CASCADE LAKE
[10]   TEMPORAL VARIATION IN A PALEOLIMNOLOGICAL RECORD ARISING FROM A TROPHIC CASCADE [J].
CARPENTER, SR ;
LEAVITT, PR .
ECOLOGY, 1991, 72 (01) :277-285