A chronology of hurricane landfalls at Little Sippewissett Marsh, Massachusetts, USA, using optical dating
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A chronology of hurricane landfalls at Little Sippewissett Marsh, Massachusetts, USA, using optical dating. / Madsen, Anni Tindahl; Duller, G.A.T.; Donnelly, J.P.; Roberts, H.M.
In: Geomorphology, Vol. 109, No. 1-2, 2009, p. 36-45.Research output: Contribution to journal › Journal article › Research › peer-review
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TY - JOUR
T1 - A chronology of hurricane landfalls at Little Sippewissett Marsh, Massachusetts, USA, using optical dating
AU - Madsen, Anni Tindahl
AU - Duller, G.A.T.
AU - Donnelly, J.P.
AU - Roberts, H.M.
PY - 2009
Y1 - 2009
N2 - Optical dating has been applied to sediments preserved in Little Sippewissett Marsh, Massachusetts, USA, which are associated with overwashing of the beach barrier during hurricane strikes on the coast. The aims were to determine the hurricane landfall frequency, and make comparisons with independent age control and the historical record. Written sources of hurricane activity along the American east coast are only considered reliable back to the mid 19th century, but the sedimentary record is potentially much longer. Optical dating was applied to quartz grains extracted from thirteen samples within a sediment core from the salt-marsh. Variability in the luminescence characteristics between aliquots was observed and ~33% of the measured aliquots were discarded based upon the ratio of the fast component to the medium component. The majority of the samples gave normal dose distributions implying homogeneous resetting of the luminescence signal at the time of deposition, but three of the samples required application of the minimum age model (MAM). Ages ranging between 20±2 and 594±38 years were obtained and are broadly in agreement with independent chronologies, thus demonstrating the potential of optical dating in this setting. The hurricane record based upon optical dating extends approximately 300 years further back in time than the official National Oceanic Atmospheric Administration (NOAA) record. The localised nature of hurricane landfalls means that it will be necessary to collect multiple cores from a number of different sites in order to build up a complete hurricane record for this part of the coast.
AB - Optical dating has been applied to sediments preserved in Little Sippewissett Marsh, Massachusetts, USA, which are associated with overwashing of the beach barrier during hurricane strikes on the coast. The aims were to determine the hurricane landfall frequency, and make comparisons with independent age control and the historical record. Written sources of hurricane activity along the American east coast are only considered reliable back to the mid 19th century, but the sedimentary record is potentially much longer. Optical dating was applied to quartz grains extracted from thirteen samples within a sediment core from the salt-marsh. Variability in the luminescence characteristics between aliquots was observed and ~33% of the measured aliquots were discarded based upon the ratio of the fast component to the medium component. The majority of the samples gave normal dose distributions implying homogeneous resetting of the luminescence signal at the time of deposition, but three of the samples required application of the minimum age model (MAM). Ages ranging between 20±2 and 594±38 years were obtained and are broadly in agreement with independent chronologies, thus demonstrating the potential of optical dating in this setting. The hurricane record based upon optical dating extends approximately 300 years further back in time than the official National Oceanic Atmospheric Administration (NOAA) record. The localised nature of hurricane landfalls means that it will be necessary to collect multiple cores from a number of different sites in order to build up a complete hurricane record for this part of the coast.
KW - Faculty of Science
KW - Optically stimulated luminescence
KW - Overwash sediments
KW - Historical records
U2 - 10.1016/j.geomorph.2008.08.023
DO - 10.1016/j.geomorph.2008.08.023
M3 - Journal article
VL - 109
SP - 36
EP - 45
JO - Geomorphology
JF - Geomorphology
SN - 0169-555X
IS - 1-2
ER -
ID: 10699305