Scott L Wing
Scott L Wing
Department of Paleobiology, National Museum of Natural History, Smithsonian Institution
Verified email at - Homepage
Cited by
Cited by
Assessing the causes of Late Pleistocene extinctions on the continents
AD Barnosky, PL Koch, RS Feranec, SL Wing, AB Shabel
Science 306 (5693), 70-75, 2004
Manual of leaf architecture
B Ellis, DC Daly, LJ Hickey, KR Johnson, JD Mitchell, P Wilf, SL Wing
Cornell University Press - NY Botanical Garden, 2009
When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal
J Zalasiewicz, CN Waters, M Williams, AD Barnosky, A Cearreta, ...
Quaternary international 383, 196-203, 2015
The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
FA McInerney, SL Wing
Annual Review of Earth and Planetary Sciences 39, 489-516, 2011
Global patterns in leaf 13C discrimination and implications for studies of past and future climate
AF Diefendorf, KE Mueller, SL Wing, PL Koch, KH Freeman
Proceedings of the National Academy of Sciences 107 (13), 5738-5743, 2010
Transient floral change and rapid global warming at the Paleocene-Eocene boundary
SL Wing, GJ Harrington, FA Smith, JI Bloch, DM Boyer, KH Freeman
Science 310 (5750), 993-996, 2005
Eocene continental climates and latitudinal temperature gradients
DR Greenwood, SL Wing
Geology 23 (11), 1044-1048, 1995
Making the case for a formal Anthropocene Epoch: an analysis of ongoing critiques
JA Zalasiewicz, Jan, Waters, Colin N. Wolfe, Alexander P. Barnosky, Anthony ...
Newsletters on Stratigraphy 50 (2), 205-226, 2017
Sensitivity of leaf size and shape to climate: global patterns and paleoclimatic applications
DJ Peppe, DL Royer, B Cariglino, SY Oliver, S Newman, E Leight, ...
New phytologist 190 (3), 724-739, 2011
Fossils and fossil climate: the case for equable continental interiors in the Eocene
SL Wing, DR Greenwood
Philosophical transactions of the royal society of London. Series B …, 1993
Paleobotanical evidence for near present-day levels of atmospheric CO2 during part of the Tertiary
DL Royer, SL Wing, DJ Beerling, DW Jolley, PL Koch, LJ Hickey, ...
Science 292 (5525), 2310-2313, 2001
Using fossil leaves as paleoprecipitation indicators: an Eocene example
P Wilf, SL Wing, DR Greenwood, CL Greenwood
Geology 26 (3), 203-206, 1998
Production of n-alkyl lipids in living plants and implications for the geologic past
AF Diefendorf, KH Freeman, SL Wing, HV Graham
Geochimica et Cosmochimica Acta 75 (23), 7472-7485, 2011
Ecological aspects of the Cretaceous flowering plant radiation
SL Wing, LD Boucher
Annual Review of Earth and Planetary Sciences 26 (1), 379-421, 1998
High plant diversity in Eocene South America: evidence from Patagonia
P Wilf, NR Cúneo, KR Johnson, JF Hicks, SL Wing, JD Obradovich
Science 300 (5616), 122-125, 2003
Sharply increased insect herbivory during the Paleocene–Eocene Thermal Maximum
ED Currano, P Wilf, SL Wing, CC Labandeira, EC Lovelock, DL Royer
Proceedings of the National Academy of Sciences 105 (6), 1960-1964, 2008
Stratigraphic and Earth System approaches to defining the Anthropocene
W Steffen, R Leinfelder, J Zalasiewicz, CN Waters, M Williams, ...
Earth's Future 4 (8), 324-345, 2016
Late Paleocene fossils from the Cerrejón Formation, Colombia, are the earliest record of Neotropical rainforest
SL Wing, F Herrera, CA Jaramillo, C Gómez-Navarro, P Wilf, ...
Proceedings of the National Academy of Sciences 106 (44), 18627-18632, 2009
Scale and diversity of the physical technosphere: A geological perspective
J Zalasiewicz, M Williams, CN Waters, AD Barnosky, J Palmesino, ...
The Anthropocene Review 4 (1), 9-22, 2017
Oxygen isotope and paleobotanical estimates of temperature and δ18O–latitude gradients over North America during the early Eocene
HC Fricke, SL Wing
American Journal of Science 304 (7), 612-635, 2004
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