The pollen flora of Quaternary sediments beneath Nantucket Shoals

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ID: 302378
1964
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Abstract
Plant microfossils occur abundantly in the silt below buff and white sand, which contains few microfossils, in a long core. Pollen of both primary and secondary (reworked Early Tertiary) origin is present, making interpretation of age and climatic conditions during deposition difficult. The available data indicate a marine depositional environment, temperate or cool-temperate climatic conditions, and origin during the Two Creeks interval.
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openalex_W2090267499 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Catharina R. Groot, J.J. Groot
Journal american journal of science
Year 1964
DOI
10.2475/ajs.262.4.488
URL
https://ajs.scholasticahq.com/article/59066.pdf
Keywords Keywords not found

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