| Reference Type | Journal (article/letter/editorial) |
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| Title | The youngest record of fossil land mammals from Antarctica; its significance on the evolution of the terrestrial environment of the Antarctic Peninsula during the late Eocene |
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| Journal | Journal of Paleontology |
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| Authors | Vizcaino, S. F. | Author |
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| Bond, M. | Author |
| Reguero, M. A. | Author |
| Pascual, R. | Author |
| Year | 1997 (March) | Volume | 71 |
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| Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0022336000039263Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 417280 | Long-form Identifier | mindat:1:5:417280:6 |
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| GUID | 0 |
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| Full Reference | Vizcaino, S. F., Bond, M., Reguero, M. A., Pascual, R. (1997) The youngest record of fossil land mammals from Antarctica; its significance on the evolution of the terrestrial environment of the Antarctic Peninsula during the late Eocene. Journal of Paleontology, 71 (2) 348-350 doi:10.1017/s0022336000039263 |
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| Plain Text | Vizcaino, S. F., Bond, M., Reguero, M. A., Pascual, R. (1997) The youngest record of fossil land mammals from Antarctica; its significance on the evolution of the terrestrial environment of the Antarctic Peninsula during the late Eocene. Journal of Paleontology, 71 (2) 348-350 doi:10.1017/s0022336000039263 |
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| In | (1997, March) Journal of Paleontology Vol. 71 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | The record of fossil land mammals from Antarctica has been restricted previously to the middle levels of the Eocene-?early Oligocene La Meseta Formation in Seymour Island, Antarctic Peninsula. This mostly shallow-marine sequence was divided informally into seven subunits (Tertiary Eocene La Meseta or TELM 1 to 7) by Sadler (1988). Land mammals, representing South American lineages of marsupials, edentates, and ungulates were recovered from TELM 3, 4, and 5 (Marenssi et al., 1994; Vizcaíno et al., 1994). The purpose of the present note is to report the discovery of a well-preserved ungulate tooth from the uppermost level of the La Meseta Formation (TELM 7) and to discuss its paleoenvironmental implications. |
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