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- W2021782743 abstract "Reef development on Gotland began in the lowest exposed unit, the Lower Visby Beds — a sequence of thin, interbedded green mudstones and mostly nodular limestones. The two reefs described were built up mainly by sediment-tolerant forms — halysitids, heliolitids and Syringopora — within which the remainder of the fauna was embedded. There was a marginal zone rich in rugosans (mostly radially disposed, their calyces pointing downslope from the reef centre) and a central/apical region where the halysitid frame gave way by degrees to one composed of favositids, heliolitids and stromatoporoids. Bryozoan genera also changed centripetally from delicate, stick-like forms to laminar and massive ones. The reefs probably had a low profile, not rising much more than one metre above the sea floor, and may have formed at or about a depth of 100 m." @default.
- W2021782743 created "2016-06-24" @default.
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- W2021782743 date "1982-09-01" @default.
- W2021782743 modified "2023-09-25" @default.
- W2021782743 title "The earliest gotland reefs: Two bioherms from the Lower Visby Beds (Upper Llandovery)" @default.
- W2021782743 cites W1997448934 @default.
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- W2021782743 doi "https://doi.org/10.1016/0031-0182(82)90078-5" @default.
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