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- W2281703345 abstract "Abstract Two crinoid pluricolumnals from Permian rocks of Timor show similar patterns of external pitting. Platycrinitid sp. preserves circular, parabolic pits that do not cross-cut between columnals, some have raised rims and at least one columnal shows a growth deformity. These pits are interpreted as the trace fossil Oichnus paraboloides Bromley. Crinoid sp. indet. has particularly dense pits cross-cutting columnals on one side of the pluricolumnal only and extending onto the contiguous limestone; it is a Holocene microkarstic solution feature. Care must be taken to separate true bioerosive trace fossils from modern microkarstic features in limestones in the tropics." @default.
- W2281703345 created "2016-06-24" @default.
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- W2281703345 date "2016-02-04" @default.
- W2281703345 modified "2023-09-26" @default.
- W2281703345 title "Trace fossils and tropical karst" @default.
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- W2281703345 doi "https://doi.org/10.1017/s0016756815000965" @default.
- W2281703345 hasPublicationYear "2016" @default.
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