Conifers are a major source of sedimentary leaf wax n-alkanes when dominant in the landscape: Case studies from the Paleogene

Author:

Schlanser Kristen M.,Diefendorf Aaron F.,West Christopher K.,Greenwood David R.,Basinger James F.,Meyer Herbert W.,Lowe Alexander J.,Naake Hans H.

Funder

Natural Sciences and Engineering Research Council of Canada

Sigma Xi

Paleontological Society

National Science Foundation

Polar Knowledge Canada

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference117 articles.

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2. Constraining paleohydrologic change during the Paleocene-Eocene Thermal Maximum in the continental interior of North America;Baczynski;Palaeogeography, Palaeoclimatology, Palaeoecology,2017

3. Floral diversity and climate change in central Colorado during the Eocene and Oligocene. Masters Thesis;Barton,2010

4. Paleoenvironment of the upper Oligocene Trbovlje coal seam (Slovenia);Bechtel;International Journal of Coal Geology,2004

5. Sedimentary geolipid records of historical changes in the watersheds and productivities of Lakes Ontario and Erie;Bourbonniere;Limnology and Oceanography,1996

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