| Reference Type | Journal (article/letter/editorial) |
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| Title | A Possible Fossil in a Graphitic Marble in the Connemara Schist, Cornamona, Co. Galway, Ireland |
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| Journal | Geological Magazine |
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| Authors | Leake, Bernard E. | Author |
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| Year | 1963 (February) | Volume | 100 |
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| Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800055035Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249257 | Long-form Identifier | mindat:1:5:249257:9 |
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| GUID | 0 |
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| Full Reference | Leake, Bernard E. (1963) A Possible Fossil in a Graphitic Marble in the Connemara Schist, Cornamona, Co. Galway, Ireland. Geological Magazine, 100 (1) 44-46 doi:10.1017/s0016756800055035 |
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| Plain Text | Leake, Bernard E. (1963) A Possible Fossil in a Graphitic Marble in the Connemara Schist, Cornamona, Co. Galway, Ireland. Geological Magazine, 100 (1) 44-46 doi:10.1017/s0016756800055035 |
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| In | (1963, February) Geological Magazine Vol. 100 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractA network texture made of graphite with calcite filling the holes is described from an area of staurolite-garnet grade of metamorphism. It is pointed out that this is the earliest texture preserved in the rock, and that it resembles a cellular structure and may therefore be of organic origin, possibly a primitive plant. At present, however, it is not certain that the structure is organic in origin. |
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