Journal
JOURNAL OF QUATERNARY SCIENCE
Volume 36, Issue 2, Pages 311-323Publisher
WILEY
DOI: 10.1002/jqs.3272
Keywords
mangrove; pollen; sea level; sedimentology
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The study found that utilizing mangrove pollen from Mahe, Seychelles would not reduce existing vertical uncertainties in Late Holocene sea-level reconstructions. However, the approach may be successful in other locations if mangrove vegetation is zoned at a more extensive lateral scale, closely associated with modern pollen rain and surface sediments, and if sedimentological conditions promote the preservation of pollen in fossil sequences.
We investigated the potential of mangrove pollen from Mahe, Seychelles, to improve existing metre-scale Late Holocene sediment-based sea-level reconstructions. Mangrove species at two mangrove sites are broadly zoned according to elevation within the tidal frame. Modern pollen rain from traps deployed for 1 year generally have a poor relationship with modern vegetation, and relatively low pollen production rates. Pollen from mangrove species that live in narrow elevation zones (e.g. Avicennia marina) are poorly represented in modern pollen rain, while pollen from mangrove species that live across a larger elevational range (e.g. Rhizophora mucronata) are relatively well represented. Pollen was found in extremely low concentrations in mangrove surface and core sediments, which inhibited further study into pollen transport and preservation. The results from this modern study demonstrate that utilizing mangrove pollen would not decrease existing metre-scale vertical uncertainties in Late Holocene sea-level reconstructions in the Seychelles. We suggest that this approach may still be successful in other locations if mangrove vegetation is (i) zoned at a more extensive lateral scale and (ii) is closely associated with modern pollen rain and surface sediments, and (iii) sedimentological conditions promote the preservation of pollen in fossil sequences.
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