aridity
; climate forcing
; community response
; Holocene
; isotopic composition
; Last Glacial Maximum
; paleoclimate
; paleoecology
; rainfall
; seasonality
; vegetation cover
; warm pool
; water stress
; Australia
; Borneo
; East Nusa Tenggara
; Greater Sunda Islands
; Indonesia
; Java
; Lesser Sunda Islands
; Sumba
; Sunda Isles
; Tracheophyta
Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States; Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States; MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany; Centre for Palynology and Paleoecology, Department of Geography and Environmental Science, Monash University, Clayton, VIC 3800, Australia; Department of Earth Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, Netherlands; Institute of Marine and Coastal Sciences, Rutgers, State University, New Brunswick, NJ 08901, United States; Department of Geology, Rutgers, State University, New Brunswick, NJ 08901, United States; ETH Zurich, 8092 Zurich, Switzerland; Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), 30655 Hannover, Germany; Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10694, United States; Eawag, Überlandstrasse 133, 8600 Dübendorf, Switzerland
Recommended Citation:
Dubois N.,Oppo D.W.,Galy V.V.,et al. Indonesian vegetation response to changes in rainfall seasonality over the past 25,000 years[J]. Nature Geoscience,2014-01-01,7(7)