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Middle Miocene Hominoid Origins
Science, 2000Ward et al . ([1][1]) ably show that samples of thickly enameled Middle Miocene hominoids that they attribute to a new genus, Equatorius , are distinct from Kenyapithecus . They fail to show, however, how Equatorius differs from Griphopithecus .
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Miocene and Post‐Miocene Proboscidea from East Africa.
The Transactions of the Zoological Society of London, 1942SUMMARY. Deinotherium (Kaup). The occurrence of Deinoiherium in Pleistocene deposits in Africa is now well known. The material from Kanam appears to belong to the species Deinotherium bozasi (Arambourg), originally described from the Omo River deposits.
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Chronicle of Miocene, Phase III: Middle Miocene Events: ABSTRACT
AAPG Bulletin, 1979Studies of climate evolution and Cenozoic cooling published in the past several years strengthen our previous paleontologic and stratigraphic models for significant refrigeration accompanied by lowered sea level during the middle Miocene (±15 to 12 m.y.B.P.). Currently, there is general acceptance of a eustatic lowering of sea level during late Miocene
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PGCE 2008, 2008
The Mid-Miocene Unconformity (MMU) is recognized throughout the South China Sea passive margin. It marks the end of rifting that created the marginal basin. It is understood to represent the break-up unconformity when active rifting gave way to sea-floor spreading in the contiguous southwest extension of the abyssal plain. Anomalies are not constrained
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The Mid-Miocene Unconformity (MMU) is recognized throughout the South China Sea passive margin. It marks the end of rifting that created the marginal basin. It is understood to represent the break-up unconformity when active rifting gave way to sea-floor spreading in the contiguous southwest extension of the abyssal plain. Anomalies are not constrained
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Geological Society of America Bulletin, 1965
The Oligocene-Miocene boundary has not been clearly defined, and its stratigraphic position in Europe is controversial. Because it is a boundary between international stratigraphic units, it should be defined by international agreement in an area with suitable fossils, preferably with planktonic foraminifera, at a horizon that can be identified widely ...
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The Oligocene-Miocene boundary has not been clearly defined, and its stratigraphic position in Europe is controversial. Because it is a boundary between international stratigraphic units, it should be defined by international agreement in an area with suitable fossils, preferably with planktonic foraminifera, at a horizon that can be identified widely ...
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2005
Memorie del Museo Civico di Storia Naturale di Verona, 2 serie, Sezione Scienze della Terra - 6 ...
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Memorie del Museo Civico di Storia Naturale di Verona, 2 serie, Sezione Scienze della Terra - 6 ...
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A new biologic paleoaltimetry indicating Late Miocene rapid uplift of northern Tibet Plateau
Science, 2022Yunfa Miao +2 more
exaly