Quantitative vertical zonation of salt-marsh foraminifera for reconstructing former sea level; an example from New Jersey, USA

Andrew C. Kemp, Benjamin P. Horton, David R. Vann, Simon E. Engelhart, Candace A. Grand Pre, Christopher H. Vane, Daria Nikitina, Shimon C. Anisfeld

Research output: Journal Publications and ReviewsRGC 21 - Publication in refereed journalpeer-review

60 Citations (Scopus)

Abstract

We present a quantitative technique to reconstruct sea level from assemblages of salt-marsh foraminifera using partitioning around medoids (PAM) and linear discriminant functions (LDF). The modern distribution of foraminifera was described from 62 surface samples at three salt marshes in southern New Jersey. PAM objectively estimated the number and composition of assemblages present at each site and showed that foraminifera adhered to the concept of elevation-dependent ecological zones, making them appropriate sea-level indicators. Application of PAM to a combined dataset identified five distinctive biozones occupying defined elevation ranges, which were similar to those identified elsewhere on the U.S. mid-Atlantic coast. Biozone A had high abundances of Jadammina macrescens and Trochammina inflata; biozone B was dominated by Miliammina fusca; biozone C was associated with Arenoparrella mexicana; biozone D was dominated by Tiphotrocha comprimata and biozone E was dominated by Haplophragmoides manilaensis. Foraminiferal assemblages from transitional and high salt-marsh environments occupied the narrowest elevational range and are the most precise sea-level indicators. Recognition of biozones in sequences of salt-marsh sediment using LDFs provides a probabilistic means to reconstruct sea level. We collected a core to investigate the practical application of this approach. LDFs indicated the faunal origin of 38 core samples and in cross-validation tests were accurate in 54 of 56 cases. We compared reconstructions from LDFs and a transfer function. The transfer function provides smaller error terms and can reconstruct smaller RSL changes, but LDFs are well suited to RSL reconstructions focused on larger changes and using varied assemblages. Agreement between these techniques suggests that the approach we describe can be used as an independent means to reconstruct sea level or, importantly, to check the ecological plausibility of results from other techniques. © 2011 Elsevier Ltd.
Original languageEnglish
Pages (from-to)26-39
JournalQuaternary Science Reviews
Volume54
DOIs
Publication statusPublished - 26 Oct 2012
Externally publishedYes

Bibliographical note

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Funding

Funding for this study was provided by NICRR grant DE-FC02-06ER64298 , NOAA grant NA110AR4310101 and NSF grant EAR-0951686 and 1052848 awarded to BPH. We thank the enthusiastic help with fieldwork of participants in the Earthwatch Student Challenge Awards Program. The US Fish and Wildlife Service are thanked for granting access to the Edwin Forsythe National Wildlife Refuge. SEE thanks the Greg and Susan Walker endowment to Prof. Robert Giegengack (University of Pennsylvania) and support from the USDA Forest Service Global Change Research Program of the Northern Research Station. CHV publishes with the permission of the Executive Director of British Geological Survey. Jerry Mead (Academy of Natural Sciences, Philadelphia) kindly provided the RTK unit. This paper is a contribution to IGCP project 588 “Preparing for coastal change” and PALSEA and is Earth Observatory of Singapore (EOS) publication number 35. We thank Adam Switzer, Craig Sloss and two anonymous reviewers for their helpful comments and suggestions.

Research Keywords

  • Cluster analysis
  • Discriminant function
  • Foraminifera
  • New Jersey
  • Quantitative paleoenvironmental reconstruction
  • Salt marsh
  • Sea level

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