2010
DOI: 10.1126/science.1185078
|View full text |Cite
|
Sign up to set email alerts
|

Onset of Convective Rainfall During Gradual Late Miocene Rise of the Central Andes

Abstract: This copy is for your personal, non-commercial The following resources related to this article are available online at www.sciencemag.org

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

10
119
1
3

Year Published

2011
2011
2016
2016

Publication Types

Select...
9
1

Relationship

3
7

Authors

Journals

citations
Cited by 156 publications
(133 citation statements)
references
References 29 publications
10
119
1
3
Order By: Relevance
“…The pattern in P. barbatus is in contrast to A. mellifera and N. vitripennis, which have a greater number of young pseudogenes. We hypothesize that the ant lineages that gave rise to P. barbatus experienced a major change in chemical ecology ≈10-30 Mya, possibly as a consequence of the increase in elevation of the Sierras and Andes to their present height (52,53). These western mountain ranges created rain shadows on their eastern sides and spawned the great American deserts.…”
Section: Resultsmentioning
confidence: 99%
“…The pattern in P. barbatus is in contrast to A. mellifera and N. vitripennis, which have a greater number of young pseudogenes. We hypothesize that the ant lineages that gave rise to P. barbatus experienced a major change in chemical ecology ≈10-30 Mya, possibly as a consequence of the increase in elevation of the Sierras and Andes to their present height (52,53). These western mountain ranges created rain shadows on their eastern sides and spawned the great American deserts.…”
Section: Resultsmentioning
confidence: 99%
“…Paleoclimate simulations using atmospheric general circulation models show that growth of mountain ranges and plateaus affects atmospheric circulation, and regional and global climate (e.g., Prell and Kutzbach, 1992;Kutzbach et al, 1993;Kitoh, 2004). Model simulations also show that changes in regional climate associated with mountain/plateau uplift have a large influence on the d 18 O w of precipitation as well as the d 18 O w lapse rate (Ehler and Poulsen, 2009;Poulsen et al, 2010). An elevation estimate of an area during a geologic period using an empirical d 18 O w vs. elevation relationship or a Rayleigh-type fractionation model would be reliable only if the climate conditions of the study area during the geologic time of interest were the same as that of today.…”
Section: Paleoelevation Implicationsmentioning
confidence: 95%
“…Further concerns include the recognition of competing influences (rather than purely surface elevation) on the stable isotopic composition used to deduce paleoelevation. For example, general circulation model simulations show that long-term climate change or the presence of large water bodies in the adjacent lowlands could also produce significant isotopic shifts in the Andean geologic record (Ehlers and Poulsen, 2009;Poulsen et al, 2010;Jeffery et al, 2012).…”
Section: Geological Problemmentioning
confidence: 99%