The methodological basis for fine-resolution, multi-proxy reconstructions of ombrotrophic peat bog surface wetness
The methodological basis for fine-resolution, multi-proxy reconstructions of ombrotrophic peat bog surface wetness
The need for Holocene peat-based palaeoclimatic records of increased temporal resolution has been widely identified in recent research. The often rapid growth rates of ombrotrophic bogs, when combined with fine-resolution (i.e. millimetre-scale) sampling, provide an as yet largely unexploited potential to derive sub-decadal palaeoclimatic data from this proxy-archive. However, multi-proxy, fine-resolution analyses require changes to standard methodologies, and the application of sampling techniques that are new to peat-based palaeoclimate research. A peat sampler was custom-built to allow precise and replicable millimetre-scale subsampling. Subsequent methodological testing revealed that, irrespective of sample thickness (i.e. resolution), halving the standard sample volume used for plant macrofossil (from 4 cm3 to 2 cm3) and testate amoebae (from 2 cm3 to 1 cm3) analyses and the sample weight used for peat humification analysis (from 0.2 g to 0.1 g dried peat) did not affect the interpretation of the results. A contiguous 1-mm sampling resolution for plant macrofossil analysis was also tested, but it was found that contiguous 5-mm samples provided a more reliable background record to fine-resolution testate amoebae and peat humification analyses. Based on these findings, a standardized and systematic methodological approach was developed, using the custom-built peat slicer to take millimetre-scale samples that provide enough sample material for both testate amoebae and peat humification analyses to be performed at 1-mm resolution. This approach will facilitate the testing of the palaeoclimatic reliability of multi-proxy, fine-resolution peat-based records.
161-174
Amesbury, Matthew J.
e71dd4f4-df90-41f1-85ea-c42c2a35e8e1
Barber, Keith E.
83d1acae-326d-4cb5-94b6-3d1dc78d64e9
Hughes, Paul D.M.
14f83168-b203-4a91-a850-8c48535dc31b
23 April 2010
Amesbury, Matthew J.
e71dd4f4-df90-41f1-85ea-c42c2a35e8e1
Barber, Keith E.
83d1acae-326d-4cb5-94b6-3d1dc78d64e9
Hughes, Paul D.M.
14f83168-b203-4a91-a850-8c48535dc31b
Amesbury, Matthew J., Barber, Keith E. and Hughes, Paul D.M.
(2010)
The methodological basis for fine-resolution, multi-proxy reconstructions of ombrotrophic peat bog surface wetness.
Boreas, 40 (1), .
(doi:10.1111/j.1502-3885.2010.00152.x).
Abstract
The need for Holocene peat-based palaeoclimatic records of increased temporal resolution has been widely identified in recent research. The often rapid growth rates of ombrotrophic bogs, when combined with fine-resolution (i.e. millimetre-scale) sampling, provide an as yet largely unexploited potential to derive sub-decadal palaeoclimatic data from this proxy-archive. However, multi-proxy, fine-resolution analyses require changes to standard methodologies, and the application of sampling techniques that are new to peat-based palaeoclimate research. A peat sampler was custom-built to allow precise and replicable millimetre-scale subsampling. Subsequent methodological testing revealed that, irrespective of sample thickness (i.e. resolution), halving the standard sample volume used for plant macrofossil (from 4 cm3 to 2 cm3) and testate amoebae (from 2 cm3 to 1 cm3) analyses and the sample weight used for peat humification analysis (from 0.2 g to 0.1 g dried peat) did not affect the interpretation of the results. A contiguous 1-mm sampling resolution for plant macrofossil analysis was also tested, but it was found that contiguous 5-mm samples provided a more reliable background record to fine-resolution testate amoebae and peat humification analyses. Based on these findings, a standardized and systematic methodological approach was developed, using the custom-built peat slicer to take millimetre-scale samples that provide enough sample material for both testate amoebae and peat humification analyses to be performed at 1-mm resolution. This approach will facilitate the testing of the palaeoclimatic reliability of multi-proxy, fine-resolution peat-based records.
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Published date: 23 April 2010
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Local EPrints ID: 151871
URI: http://eprints.soton.ac.uk/id/eprint/151871
ISSN: 0300-9483
PURE UUID: ab6b2ce9-b87f-457f-89b6-aa6b3b54749d
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Date deposited: 12 May 2010 14:44
Last modified: 14 Mar 2024 02:42
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Author:
Matthew J. Amesbury
Author:
Keith E. Barber
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