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Pollen
Stratigraphic Correlation and Dating of Barrier-beach Peat Sections
Clark,
J.S., J.T. Overpeck, T. Webb III, and W.A. Patterson III
1986 Review of Palaeobotany and Palynology 47: 145-168
ABSTRACT
Coastal researchers use data from core sections to reconstruct past
sedimentary environments and barrier-beach dynamics over the last 350 years.
Disjunct organic and silt strata separated by sand deposits represent former
salt marshes and lagoons that were buried in the normal course of barrier migration
processes. Interpretations are invariably limited by a lack of close time control
needed to correlate sections and to tie stratigraphic evidence to documented
changes in sea level, storms, inlet activity, overwash, and human disturbances.
Regional pollen spectra from organic and silt strata in a large number of barrier-beach
cores have been matched with spectra from a 210Pb and pollen-dated reference
profile from the centre of the study area on Great South Beach, Long Island,
New York, U.S.A. The dramatic vegetation changes following European settlement
allowed for a high degree of vertical (and thus, temporal) resolution in profiles
of regional pollen. For visual matching of pollen samples, percentages of agricultural-indicator
types, the percentages of all regional types, stratigraphic relationships,
and sediment concentrations of industrially-derived opaque spherules were considered.
Chord-distance comparisons that measure the degree of dissimilarity between
pairs of pollen spectra, produced the same correlations as visual estimates
for 80-87% of the comparisons between spectra of post-settlement age (i.e.
spectra containing agricultural indicators).
These correlations were used to establish isochrones through a transect of
cores across the barrier beach. 210Pb provided an absolute chronology for a
reconstruction of geomorphic events that included inlet changes, overwash,
and salt-marsh formation. The advantages of the present methods for both absolute
dating and chronostratigraphic correlation were evident when the age estimates
derived from pollen data were compared to 29 14C dates.
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