Terrestrial fossils in the marine Presumpscot Formation: implications for Late Wisconsinan paleoenvironments and isostatic rebound along the coast of Maine

Scott R Anderson, N. G. Miller, R. B. Davis, R. E. Nelson

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

Investigations of terrestrially derived organic remains within the late-glacial marine Presumpscot Formation near Portland, Maine, adds one new shrub species, six moss species, and representatives of six families of insects to the fossil biota of the deposit. White spruce (Picea glauca) dominates the plant macrofossil assemblage; the dominant pollen type is also spruce. The total biotic assemblage probably represents remnants of a forest-floor litter layer, eroded along a stream and subsequently deposited offshore. Three accelerator mass spectrometer (AMS) dates on spruce needles and cones suggest rapid burial, with marine regression from the area by c 11 500 BP. -Authors

Original languageEnglish (US)
Pages (from-to)1241-1246
Number of pages6
JournalCanadian Journal of Earth Sciences
Volume27
Issue number9
StatePublished - 1990

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paleoenvironment
fossil
coast
late glacial
forest floor
moss
biota
litter
spectrometer
shrub
pollen
insect
family

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Terrestrial fossils in the marine Presumpscot Formation : implications for Late Wisconsinan paleoenvironments and isostatic rebound along the coast of Maine. / Anderson, Scott R; Miller, N. G.; Davis, R. B.; Nelson, R. E.

In: Canadian Journal of Earth Sciences, Vol. 27, No. 9, 1990, p. 1241-1246.

Research output: Contribution to journalArticle

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