A new <i>Carbonicola</i> band in the lower coal measures of helpet edge, near rochdale

Ashton, Hannah; Cowgill, Jane; Eagar, K. M. C.

doi:10.1002/gj.3350010302

Cited by 3 publications

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References 2 publications

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“…(Tonks and others 1931, p. 134; Wright 1934a, p. 21; Jones and others 1938, p. 79). It is proposed here to refer only to the thick strongly developed band of shells, well known to the Geological Survey, which has been found usually about 60 feet below the Arley Mine over a wide area and which constitutes the a recent-publication, has suggested that this nanic is more suitable for it (Eagar 1954 , p. 56). A fauna from 60 to 75 feet below thc Arley Mine (Fig.…”

Section: (F) the Carbonicolu T O M Bandmentioning

confidence: 99%

Additions to the non‐marine fauna of the lower coal measures of the North‐Midlands Coalfields

Eagar¹

1954

Geological Journal

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The main elements of the non-marine fauna are reviewed in stratigraphical order in the light of recent revisional work on the Anthracosiidae. -4ttention is directed towards non-marine facies and to the lesser known faunas from the upper half of the Lower Coal Measures, from which Carbonicola cxtcnuata and C . pom'ma spp. nov. are described. Evidence is adduced to suggest that the boundary between the lenisulcda and communis Zones, defined by Wray and Trueman (1934)

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Section: (F) the Carbonicolu T O M Bandmentioning

confidence: 99%

Additions to the non‐marine fauna of the lower coal measures of the North‐Midlands Coalfields

Eagar¹

1954

Geological Journal

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A Guide to the Geology of the Cliviger Valley, Near Burnley, Lancashire

Williamson

1956

PYGS

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Distribution of Westphalian Marine Faunas in Northern England and Adjoining Areas

Calver

1968

PYGS

120

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Summary The main features of the Westphalian marine faunas in the coalfields of the Pennine Province are summarized by reference to the sequence proved in the East Midlands Coalfield, which is taken as a standard for the region. The faunal phases of the marine bands are described and the possible spatial relationship of the communities in the Westphalian seas is discussed in terms of facies belts. The geographical distribution of the communities in the marine bands is set out, and interpreted by palaeofacies maps. These demonstrate the lateral changes which occur in the faunas as the individual bands are traced from the area of maximum deposition in the mid and south Pennines to the surrounding marginal areas. The pattern of the faunal variation is seen to be in close agreement with the depositional history and palaeogeography of the Pennine basin. Brief reference is made to the position of the permanent Westphalian seas.

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A new Carbonicola band in the lower coal measures of helpet edge, near rochdale

Cited by 3 publications

References 2 publications

Additions to the non‐marine fauna of the lower coal measures of the North‐Midlands Coalfields

Additions to the non‐marine fauna of the lower coal measures of the North‐Midlands Coalfields

A Guide to the Geology of the Cliviger Valley, Near Burnley, Lancashire

Distribution of Westphalian Marine Faunas in Northern England and Adjoining Areas

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