Occurrence and preservation of Eocene squamariacean and coralline rhodoliths: Eau, Tonga

Binyamin Buchbinder; Robert B. Halley

doi:10.1007/978-3-642-70355-3_19

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Occurrence and preservation of Eocene squamariacean and coralline rhodoliths: Eau, Tonga

Binyamin Buchbinder·Robert B. Halley

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Abstract

A widespread rhodolith facies occurs within middle Eocene limestones of Eua, Tonga (Fig. 1). These limestones, first described by Hoffmeister (1932), represent a portion of a broad, early Tertiary platform that developed in the Tonga area prior to disruption and uplift by later Tertiary plate movements (Kroenke and Tongilava 1975). Algal rhodoliths form beds several meters thick within Eocene limestones and occur at localities several kilometers apart along the length of Eua.

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Source-reported bounding extent: -21.478629309978384° to -21.268899719967695° latitude; -175.05889892578125° to -174.83917236328125° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Binyamin Buchbinder, Robert B. Halley. 1985. Occurrence and preservation of Eocene squamariacean and coralline rhodoliths: Eau, Tonga. https://doi.org/10.1007/978-3-642-70355-3_19

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