Relationship between peat geochemistry and depositional environments, Cranberry Island, Maine

International Journal of Coal Geology
By: , and 

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Abstract

The Heath, Great Cranberry Island, Maine, offers a unique locality for studying lateral and vertical relationships between radically different peat types within 1 km2. The majority of The Heath is a Sphagnum moss-dominated raised bog. Surrounding the raised bog is a swamp/marsh complex containing grass, sedge, Sphagnum moss, alder, tamarack, and skunk cabbage. Swamp/ marsh-deposited peat occurs both around the margins of The Heath and under Sphagnum-dominated peat, which was deposited within the raised bog. A third peat type, dominated by herbaceous aquatics, is present underlying the swamp/marsh-dominated peat but is not present as a dominant botanical community of The Heath. The three peat types have major differences in petrographic characteristics, ash contents, and associated minerals. Sulfur contents range from a low of 0.19 wt.% (dry) within the raised bog to a high of 4.44 wt% (dry) near the west end of The Heath, where swamp/marsh peat occurring directly behind a storm beach berm has been influenced by marine waters. The presence of major geochemical variations within a 1-km2 peat deposit suggests the need for in-depth characterization of potential peat resources prior to use.




Publication type Article
Publication Subtype Journal Article
Title Relationship between peat geochemistry and depositional environments, Cranberry Island, Maine
Series title International Journal of Coal Geology
DOI 10.1016/0166-5162(87)90030-9
Volume 8
Issue 1-2
Year Published 1987
Language English
Publisher Elsevier
Description 13 p.
First page 175
Last page 187
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