Results 91 to 100 of about 34,573 (203)
Plant and associated insect-damage diversity in the western U.S.A. decreased significantly at the Cretaceous-Paleogene (K-Pg) boundary and remained low until the late Paleocene. However, the Mexican Hat locality (ca.
Michael P Donovan +4 more
doaj +1 more source
Morphology and anatomy of the extinct angiosperm fruit, Porosia verrucosa (Lesqueruex) Hickey, are documented in detail based on various modes of preservation including molds, casts, and permineralizations from more than seventy localities in the late ...
Manchester Steven R., Kodrul Tatyana M.
doaj +1 more source
Resolving the relationships of Paleocene placental mammals.
The 'Age of Mammals' began in the Paleocene epoch, the 10 million year interval immediately following the Cretaceous-Palaeogene mass extinction. The apparently rapid shift in mammalian ecomorphs from small, largely insectivorous forms to many small-to-large-bodied, diverse taxa has driven a hypothesis that the end-Cretaceous heralded an adaptive ...
Halliday, TJD, Upchurch, P, Goswami, A
openaire +3 more sources
Impact ejecta at the Paleocene-Eocene boundary
An impactful event Glassy silica spherules have been found in marine sediments from three sites across a wide area off the Atlantic coast of the United States, near the stratigraphic level of the Paleocene-Eocene boundary.
Schaller, Morgan +4 more
openaire +4 more sources
UPPER CRETACEOUS AND PALEOCENE IN ZANSKAR RANGE (NW Himalaya)
A detailed Upper Cretaceous/Paleocene stratigraphic section was measured from the Spanboth Chu Valley, High Himalaya Nappes. Placement Of the Cretaceous—Tertiary boundary was refined, but some uncertitudes still remain because of poor exposure in this ...
MAURIZIO GAETANI +5 more
doaj
Magnetostratigraphy of the Hell Creek and lower Fort Union formations in northeast Montana [PDF]
Magnetostratigraphic evaluation of a well-exposed stratigraphic section in northeast Montana has been undertaken to expand upon and better understand the timing of the deposition of Hell Creek and Fort Union Formations.
LeCain, Rebecca
core +2 more sources
A foreland basin is a dynamic system whose depositional systems migrate in response to changes in tectonic uplift patterns, sedimentary filling processes and isostatic rebound of the lithosphere. The Paleocene-middle Miocene foreland system of the Llanos
German Bayona +4 more
doaj
N. O. Holst, Karl A. Grönwall
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Substantial continental temperature rise over the Paleocene-Eocene Thermal Maximum in the Pyrenees
The Eocene period experienced several hyperthermal events with the Paleocene-Eocene Thermal Maximum being the most significant. During this event, global mean surface temperatures were 5–6 °C higher and latitudinal temperature gradients were reduced ...
Gábor Újvári +10 more
doaj +1 more source
The succession of the Maiella massif is analyzed, focusing on the colonial-coral bearing deposits occurring just below and immediately above the Cretaceous/Paleogene boundary.
Giovanni Coletti +11 more
doaj +1 more source

