An analysis of modern pollen rain on an elevational gradient in southern Peru

By C. Weng, Mark Bush, M. Silman. Journal of Tropical Ecology, 2004

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Differentiation between neotropical rainforest, dry forest, and savannah ecosystems by their modern pollen spectra and implications for the fossil pollen record. (2009, unknown): “Although the number of modern pollen rain studies of Neotropical METF 22 (Bush, 1991; Behling et al., 1997; Behling and da Costa, 2000; Bush, 2000; Bush et al., 23 2001; Bush and Rivera, 2001; Weng et al., 2004; Gosling et al., 2005), SDTF 24 (Grabandt, 1980; Rodgers III and Horn, 1996; Bush and Riv”
The influence of climate on the spatial patterning of Neotropical plant families (2007, background): “Similarly, the abundance of Rubiaceae, known to be abundant in mid-elevation forests (Weng et al., 2004), covaries negatively with temperature, while the number of species at a given site covaries positively with precipitation.”
Introducing a new (freeware) tool for palynology (2007, background): “In those areas, traps were set in permanent vegetation quadrats at La Selva (Costa Rica), Cuyabeno (Ecuador), Barro Colorado Island (Panama) and the Biological Diversity of Forest Fragments Project in Brazilian Amazonia (Bush, 2000; Bush et al., 2001; Weng et al., 2004).”