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On the Erosive Trail of A 14Th and 15Th Century Hurricane in Connecticut (Usa) Salt Marshes

Published online by Cambridge University Press:  18 July 2016

O VAN de Plassche ,
A J Wright ,
K VAN der Borg  and
F A M de Jong
O VAN de Plassche*
Affiliation:
Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands
A J Wright
Affiliation:
Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands
K VAN der Borg
Affiliation:
R J van der Graaff Laboratory, Universiteit Utrecht, P.O. Box 80.000, 3508 TA, the Netherlands
F A M de Jong
Affiliation:
R J van der Graaff Laboratory, Universiteit Utrecht, P.O. Box 80.000, 3508 TA, the Netherlands
*
Corresponding author. Email: orson.van.de.plassche@falw.vu.nl.
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Abstract

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This paper examines if an erosive hiatus found in the peat stratigraphy and marsh-accumulation record from northwest Hammock River Marsh (HRM), Connecticut (CT) can be attributed to a 14th or a 15th century hurricane, each documented by a radiocarbon-dated overwash fan in Succotash Marsh (SM) (Rhode Island) about 90 km to the east. Given that (i) the best estimate age range for the 15th century overwash deposit in SM (1400–1440 cal AD, 2 σ) overlaps entirely with that for first plant growth after erosion at HRM (1390–1450 cal AD, 2 σ), while the best estimate age range for the 14th century overwash deposit (1290–1410 cal AD, 2 σ) overlaps just 10 yr, and (ii) interpretation of the available stratigraphic and sedimentary evidence from HRM suggests that a high-energy event offers the simplest explanation for the observed marsh erosion, we conclude that a plausible link exists between the 15th century hurricane and the marsh erosion in HRM. The best estimate age range for the 14th century hurricane appears to overlap for 91% with the age range for the first plant growth (1290–1400 cal AD, 2 σ) following marsh erosion in East River Marsh (CT), located about 12 km west of HRM. These results imply that erosive boundaries in salt-marsh peat deposits have potential as markers of past hurricane activity.

Type
Part II
Information
Radiocarbon , Volume 46 , Issue 2: Proceedings of the 18th International Radiocarbon Conference (Part 2 of 2), Conference Editors: Nancy Beavan Athfield, Rodger J Sparks , 2004 , pp. 775 - 784
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Bertness, MD. 1991. Zonation of Spartina patens and Spartina alterniflora in a New England salt marsh. Ecology 72:138–48.CrossRefGoogle Scholar
Boose, ER, Chamberlin, KE, Foster, DR. 2001. Landscape and regional impacts of hurricanes in New England. Ecological Monographs 71(1):27–48.CrossRefGoogle Scholar
Bronk Ramsey, C. 1995. Radiocarbon calibration and analysis of stratigraphy: the OxCal program. Radiocarbon 37(2):425–30.CrossRefGoogle Scholar
Donnelly, JP, Bryant, SM, Butler, J, Dowling, J, Fan, L, Hausmann, N, Newby, P, Shuman, B, Stern, J, Westover, K, Webb, T. III 2001a. 700 yr sedimentary record of intense hurricane landfalls in southern New England. Geological Society of America Bulletin 113(6):714–27.2.0.CO;2>CrossRefGoogle Scholar
Donnelly, JP, Roll, S, Wengren, M, Butler, J, Lederer, R, Webb, T. III 2001b. Sedimentary evidence of intense hurricane strikes from New Jersey. Geology 29(7): 615–8.2.0.CO;2>CrossRefGoogle Scholar
Niering, WA, Warren, RS. 1980. Vegetation patterns and processes in New England salt marshes. Bioscience 30:301–7.CrossRefGoogle Scholar
Nyman, JA, Crozier, CR, Delaune, RD. 1995. Roles and patterns of hurricane sedimentation in an estuarine marsh landscape. Estuarine Coastal and Shelf Science 40:665–79.CrossRefGoogle Scholar
Stuiver, M, Reimer, PJ, Bard, E, Beck, JW, Burr, GS, Hughen, KA, Kromer, B, McCormac, FG, van der Plicht, J, Spurk, M. 1998. INTCAL98 radiocarbon age calibration: 24,000–0 BP. Radiocarbon 40(3):1041–83.CrossRefGoogle Scholar
van de Plassche, O, van der Borg, K, de Jong, AFM. 1998. Sea level-climate correlation during the past 1400 yr. Geology 26:319–22.2.3.CO;2>CrossRefGoogle Scholar
van de Plassche, O, van der Borg, K, de Jong, AFM. 2002. Relative sea-level rise across the Eastern Border fault (Branford, Connecticut): evidence against seismotectonic movements. Marine Geology 184:61–8.CrossRefGoogle Scholar
van de Plassche, O, Edwards, RJ, van der Borg, K, de Jong, AFM. 2001. 14C wiggle-match dating in high-resolution sea-level research. Radiocarbon 43(2A):391–402.CrossRefGoogle Scholar
Varekamp, JC, Thomas, E, van de Plassche, O. 1992. Relative sea-level rise and climate change over the last 1500 years (Clinton, CT, USA). Terra Nova 4: 293–304.CrossRefGoogle Scholar
Warren, RS, Niering, WA 1993. Vegetation change on a northeast tidal marsh: interaction of sea-level rise and marsh accretion. Ecology 74:96–103.CrossRefGoogle Scholar