Mark Bush

Dr. Mark Bush


Research Focus & Metrics

Academic Career Length

40Years (1987-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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20 February 2007 in Ecology Letters
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Journal Article
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GMGary G. Mittelbach
Gary G. Mittelbach
DSDouglas W. Schemske
Douglas W. Schemske
HCHoward V. Cornell
Howard V. Cornell
AAAndrew Allen
Andrew Allen
JBJonathan M. Brown
Jonathan M. Brown
MTMichael Turelli
Michael Turelli

14 December 2007 in Climate Dynamics
Verified
Journal Article
Closed access
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MPM. J. Power
M. J. Power
JMJ. Marlon
J. Marlon
NON. Ortiz
N. Ortiz
PBP. J. Bartlein
P. J. Bartlein
SHSandy Harrison
Sandy Harrison
JZJiahua Zhang
Jiahua Zhang

4 October 1996 in Science
Verified
Journal Article
Closed access
PCP. A. Colinvaux
P. A. Colinvaux
POP. E. De Oliveira
P. E. De Oliveira
JMJ. E. Moreno
J. E. Moreno
MMM. C. Miller
M. C. Miller
MBMark Bush
Mark Bush
A continuous pollen history of more than 40,000 years was obtained from a lake in the lowland Amazon rain forest. Pollen spectra demonstrate that tropical rain forest occupied the region continuously and that savannas or grasslands were not present during the last glacial maximum. The data suggest that the western Amazon forest was not fragmented into refugia in glacial times and that the lowlands were not a source of dust. Glacial age forests were comparable to modern forests but also included species now restricted to higher elevations by temperature, suggesting a cooling of the order of 5° to 6°C.

31 August 2018 in Science
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Journal Article
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CNConnor Nolan
Connor Nolan
JOJonathan T. Overpeck
Jonathan T. Overpeck
JAJudy R. M. Allen
Judy R. M. Allen
PAPatricia M. Anderson
Patricia M. Anderson
JBJulio L. Betancourt
Julio L. Betancourt
SJStephen T. Jackson
Stephen T. Jackson
Future predictions from paleoecology: Terrestrial ecosystems will be transformed by current anthropogenic change, but the extent of this change remains a challenge to predict. Nolan et al. looked at documented vegetational and climatic changes at almost 600 sites worldwide since the last glacial maximum 21,000 years ago. From this, they determined vegetation responses to temperature changes of 4° to 7°C. They went on to estimate the extent of ecosystem changes under current similar (albeit more rapid) scenarios of warming. Without substantial mitigation efforts, terrestrial ecosystems are at risk of major transformation in composition and structure. Science , this issue p. 920

1 January 2000 in Quaternary Science Reviews
Verified
Journal Article
Closed access
PCP.A. Colinvaux
P.A. Colinvaux
POP.E. De Oliveira
P.E. De Oliveira
MBMark Bush
Mark Bush

22 December 2010 in Journal of Biogeography
Verified
Journal Article
Closed access
PDF file
KFKenneth J. Feeley
Kenneth J. Feeley
MSMiles R. Silman
Miles R. Silman
MBMark Bush
Mark Bush
WFWILLIAM FARFAN-RIOS
WILLIAM FARFAN-RIOS
KCKarina Garcia Cabrera
Karina Garcia Cabrera
SSSassan Saatchi
Sassan Saatchi