Abstract
Shallow lakes are among the most threatened ecosystems in the world and many contemporary studies have demonstrated declines in biodiversity due to anthropogenic forcing. Mostly, however, these studies have not covered the full period of human-induced diversity change in lakes which is typically over decades-centuries. Here we provide two examples of palaeoecological studies focussed on reconstructing biodiversity changes in contrasting shallow lake environments that demonstrate the efficacy of the approach—a shallow UK lake and a suite of floodplain lakes (called billabongs) in the Murray-Darling basin, Australia. In the Murray-Darling billabongs, complex sedimentary processes operate, sediment chronologies are less certain and replication of sites is needed to confirm patterns. The combination of sediment records from 10 billabongs showed that diatom diversity changes pre- and post-European (>1850) disturbance were inconsistent; however, reductions in diversity were more common and appear to reflect reductions in macrophyte abundance. At Felbrigg Lake, a multi-proxy study with strong chronological control demonstrated divergent responses of macrophyte, diatom, cladoceran and chironomid richness and diversity to a century of eutrophication. Eutrophication of the site was qualitatively inferred from changes in the macrophyte community in turn reconstructed from plant macrofossils. Benthic cladocerans showed a consistent decline in richness through the record, reflecting the gradual reduction in their macrophyte associated habitat over the past century. Diatom richness and diversity responses were complex, with increases in diversity and richness linked to both increases and decreases in macrophyte species richness and abundance. Chironomid richness and diversity patterns were less consistently linked to eutrophication. The loss of the dominant zooplanktivore (perch) in the 1970s was reflected in the richness and diversity profiles for all groups. Our study reveals clear potential for using sediment cores to infer biodiversity change in shallow lakes and shallow lake regions. However, given the contrasting patterns of diversity change for the different biological groups both in Felbrigg Lake and between Felbrigg and the billabongs, caution is required when interpreting whole-ecosystem biodiversity changes (or the absence of change) based on single as opposed to multi-proxy studies.
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Acknowledgments
We thank the National Trust for supporting our work at Felbrigg Lake, the ARC and University of New England for supporting research at the Australian billabongs and two anonymous reviewers for very useful and supportive comments. We also thank Amy Burgess and Pete Langdon for contributing data. This paper was written with support to CS from the European Union FP7 project ‘BIOFRESH’ (Contract No. 226874). TD’s contribution was supported by the Center for Informatics Research on Complexity in Ecology (CIRCE), funded by the Aarhus University Research Foundation under the AU Ideas program. This is PuBoPeD publication number 46. We would like to take this opportunity to express our gratitude to Rick Battarbee for his inspirational support, encouragement and enthusiasm over the years.
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A celebration of Prof Rick Battarbee’s contributions to palaeolimnology, edited by Holmes et al.
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Davidson, T.A., Reid, M.A., Sayer, C.D. et al. Palaeolimnological records of shallow lake biodiversity change: exploring the merits of single versus multi-proxy approaches. J Paleolimnol 49, 431–446 (2013). https://doi.org/10.1007/s10933-013-9696-8
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DOI: https://doi.org/10.1007/s10933-013-9696-8
Keywords
- Shallow Lakes
- Biodiversity
- Palaeoecology
- Diatoms
- Cladocera
- Submerged
- Plants