UO Data

Permanent URI for this collection

https://hdl.handle.net/1794/12310

Browse

Browsing UO Data by Subject "Cenozoic"

Now showing 1 - 2 of 2
  • ItemRestricted
    Data for Cenozoic paleoclimate on land in North America
    (University of Oregon, 2016-04) Retallack, Greg J.
    Paleotemperature and paleoprecipitation over the past 40 m.yr. can be inferred from the degree of chemical weathering and depth of carbonate nodules in paleosols of Oregon, Montana, and Nebraska. Paleosol records show that late Eocene (35 Ma), middle Miocene (16 Ma), late Miocene (7 Ma), and early Pliocene (4 Ma) warm climatic episodes were also times of a wet climate in Oregon, Montana, and Nebraska. Oregon and Nebraska were humid during warmwet times, but Montana was no wetter than subhumid within the rain shadow of intermontane basins. Global warmwet paleoclimatic spikes steepened rather than flattened geographic gradients of Rocky Mountain rain shadows. Longlived mountain barriers created dusty dry basins with sedimentation rates high enough to preserve Milankovitch-scale (100–41 kyr) global paleoclimatic variation in some sequences of paleosols. Greenhouse warm-wet climates indicated by paleosols were also peaks of diversity for North American plants and animals and coincided with advances in coevolution of grasses and grazers. Paleosol records differ from global compilations of marine foraminiferal oxygen and carbon isotopic composition, due to competing influences of global ice volume and C4 grass expansion. Paleosol records support links between global warming and high atmospheric CO2.
  • ItemOpen Access
    Paleosol data from Kenya.
    (2016-11-21) Retallack, Greg J.
    Data collected in several areas of Kenya with Cenozoic deposits well known for fossil mammals, including islands and shores of Lake Victoria, the central and southern Gregory Rift, and the basin of Lake Turkana. Data are largely measurements of key characteristics of fossil soils (paleosols) in the field: depth to the carbonate (Bk) horizon, thickness of the carbonate (Bk) horizon and size of the carbonate nodules.