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The Southern Andes, stretching from the subtropics to the subantarctic, are ideally located for palaeoenvironmental research. Over the broad and continuous latitudinal extent of the cordillera (-24˚), vegetation is adjusted to climatic gradients and atmospheric circulation patterns. Opposed to the prevailing Southern Westerlies, the Southern Andes are positioned to receive the brunt of the winds, while biota are set to record the shifting of incoming storm systems over time. Sequential, latitudinally-placed, sedimentary deposits containing microfossils and macroremains, as a
Paleoecology --- Paleoecology --- Paleoecology --- Paleoecology --- Glacial epoch --- Glacial epoch --- Glacial epoch
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Paleontology --- Geology, Stratigraphic --- Paleoecology --- Paleolimnology --- Glacial epoch
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Biosphere --- Evolution (Biology) --- Natural history --- Paleoecology
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Evolutionary paleoecology. --- Evolution (Biology). --- Expanding universe. --- Eye
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Sherry V. Nelson examines the adaptations and extinction of Sivapithecus , a Miocene hominoid, in the Siwaliks of Pakistan. Three different studies involving dental microwear and stable isotopic analyses are interwoven to provide reconstructions of the preferred landscape, climate, and diet of Sivapithecus as well as changes in the environment that led to its extinction. This book presents new techniques that allow for a more detailed analysis of faunal and environmental change than ever before documented for an ape clade throughout its radiation and demise.
Animal remains (Archaeology) --- Paleoecology --- Sivapithecus --- Teeth, Fossil
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Antiquities, Prehistoric --- Archaeology --- Excavations (Archaeology) --- Paleoecology --- Portugal --- Antiquities.
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How did life begin? What was 'snowball earth'? Why did the dinosaurs become extinct? Are we all descended from 'African Eve'? Will humans be responsible for the next major extinction? These and many other fundamental questions are addressed in this masterly account of The Story of Life, by eminent biologist and teacher Richard Southwood.The story unfolds with the formation of the earth around four thousand million years ago. Life first emerged a hundred million years later, and it took another fifteen million years for more complex life-forms to appear. Periods of relative calm were punctuated
Biology --- Evolution (Biology) --- History. --- Evolution (Biology). --- Extinction (Biology). --- Paleoecology. --- BIOLOGY --- HISTORY
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The Southern Andes, stretching from the subtropics to the subantarctic, are ideally located for palaeoenvironmental research. Over the broad and continuous latitudinal extent of the cordillera (-24˚), vegetation is adjusted to climatic gradients and atmospheric circulation patterns. Opposed to the prevailing Southern Westerlies, the Southern Andes are positioned to receive the brunt of the winds, while biota are set to record the shifting of incoming storm systems over time. Sequential, latitudinally-placed, sedimentary deposits containing microfossils and macroremains, as a
Paleoecology --- Glacial epoch --- Ice Age --- Geology, Stratigraphic --- Palaeoecology --- Ecology --- Paleobiology --- Pleistocene Epoch
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