The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site; discussion

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doi: 10.1016/j.quascirev.2014.08.014
Author(s): Naafs, B. D. A.; Martínez-García, A.; Grützner, J.; Higgins, S.
Author Affiliation(s): Primary:
University of Bristol, School of Chemistry, Bristol, United Kingdom
Other:
Eidgenössische Technische Hochschule Zürich, Switzerland
Alfred Wegener Institute for Polar and Marine Research, Germany
Lamont-Doherty Earth Observatory, United States
Volume Title: Quaternary Science Reviews
Source: Quaternary Science Reviews, Vol.103, p.175-179. Publisher: Elsevier, International. ISSN: 0277-3791
Note: In English. For reference to original see Lang, D. et al., Quat. Sci. Rev., Vol. 93, p. 125-141, 2014. 13 refs.; illus.
Year of Publication: 2014
Research Program: IODP Integrated Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Aliphatic hydrocarbons; Alkanes; Atlantic Ocean; Biomarkers; C-13/C-12; Calcium carbonate; Carbon; Carbonates; Cenozoic; Chemostratigraphy; Clastic sediments; Cores; Dust; Expedition 306; Expeditions 303/306; Glacial environment; Hydrocarbons; IODP Site U1313; Integrated Ocean Drilling Program; Interglacial environment; Isotope ratios; Isotopes; Lithostratigraphy; Marine sediments; Mid-Atlantic Ridge; Neogene; North Atlantic; O-18/O-16; Organic compounds; Oxygen; Pleistocene; Pliocene; Quaternary; Sediments; Stable isotopes; Terrigenous materials; Tertiary
Coordinates: N410000 N410000 W0325700 W0325700
Record ID: 2015013462
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands