A common opportunistic foraminiferal species as an indicator of rapidly changing conditions in a range of environments

被引:91
作者
Alve, E [1 ]
机构
[1] Univ Oslo, Dept Geol, N-0316 Oslo, Norway
关键词
hydrographic fronts; physical disturbance; ephemeral dysoxia/anoxia; trawling; Stainforthia fusiformis (Williamson); environmental change;
D O I
10.1016/S0272-7714(02)00383-9
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Long-term biological and environmental time-series (several decades to centuries) are essential for distinguishing between anthropogenically and naturally induced environmental change as well as for monitoring environmental change over time, irrespective of the causes. Since such long time-series are virtually non-existent for most areas, other methods have to be explored which can provide the best possible analogues. Numerous investigations have shown that benthic foraminifera (meiofaunal protists), which leave a fossil record in most marine sediments, are well suited for this purpose. A prerequisite for performing sound interpretations is an optimal understanding of their biology and ecology. Stainforthia fusiformis (Williamson) is one of the most common benthic foraminiferal species in NW European waters and living (stained) populations have been recorded in all clastic, soft bottom intertidal to outer shelf and slope areas with sediments consisting of at least some fines (>4% <63 mum) as long as the salinity is >28. Its predominance in ephemerally dysoxic/anoxic areas has caused it to be used as a proxy for severe oxygen depletion. A strong dominance (even >90%) of this species is, however, also reported from well-oxygenated coastal and shelf settings and, consequently, high abundance of this species occurs in habitats with very different environmental characteristics. A closer examination of these areas suggests that they can be roughly grouped into three categories: (1) beneath hydrographic frontal areas, (2) physically disturbed areas of sediment, and (3) ephemerally dysoxic/anoxic basins. The main characteristic feature that these highly different environments have in common is that they experience rapidly changing conditions. It is concluded that the opportunistic life-strategy of S. fusiformis makes it highly adapted to cope with environmental stress and that this, rather than tolerance to a particular environmental parameter, causes it to predominate in areas subject to rapidly changing environmental conditions. (C) 2003 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:501 / 514
页数:14
相关论文
共 99 条
[1]   BENTHIC FORAMINIFERAL DISTRIBUTION AND RECOLONIZATION OF FORMERLY ANOXIC ENVIRONMENTS IN DRAMMENSFJORD, SOUTHERN NORWAY [J].
ALVE, E .
MARINE MICROPALEONTOLOGY, 1995, 25 (2-3) :169-186
[2]   High benthic fertility and taphonomy of foraminifera: a case study of the Skagerrak, North Sea [J].
Alve, E ;
Murray, JW .
MARINE MICROPALEONTOLOGY, 1997, 31 (3-4) :157-175
[3]   Benthic foraminiferal distribution and abundance changes in Skagerrak surface sediments: 1937 (Hoglund) and 1992/1993 data compared [J].
Alve, E ;
Murray, JW .
MARINE MICROPALEONTOLOGY, 1995, 25 (04) :269-288
[4]  
Alve E., 1991, Holocene, V1, P243, DOI 10.1177/095968369100100306
[5]   Resting stage in benthic foraminiferal propagules: a key feature for dispersal? Evidence from two shallow-water species [J].
Alve, E ;
Goldstein, ST .
JOURNAL OF MICROPALAEONTOLOGY, 2002, 21 :95-96
[6]   VERTICAL MIGRATORY RESPONSE OF BENTHIC FORAMINIFERA TO CONTROLLED OXYGEN CONCENTRATIONS IN AN EXPERIMENTAL MESOCOSM [J].
ALVE, E ;
BERNHARD, JM .
MARINE ECOLOGY PROGRESS SERIES, 1995, 116 (1-3) :137-151
[7]   Temporal variability in vertical distributions of live (stained) intertidal foraminifera, southern England [J].
Alve, E ;
Murray, JW .
JOURNAL OF FORAMINIFERAL RESEARCH, 2001, 31 (01) :12-24
[8]   Colonization of new habitats by benthic foraminifera: a review [J].
Alve, E .
EARTH-SCIENCE REVIEWS, 1999, 46 (1-4) :167-185
[9]  
Alve E., 1996, Nor. Geol. Unders. Bull., V430, P85
[10]  
ALVE E, 2000, ENV MICROPALEONTOLOG, P323