Regional insight into savanna hydrogeomorphology from termite mounds.
Global vegetation models predict the spread of woody vegetation in African savannas and grasslands under future climate scenarios, but they operate too broadly to consider hillslope-scale variations in tree-grass distribution. Topographically linked hydrology-soil-vegetation sequences, or catenas, underpin a variety of ecological processes in savannas, including responses to climate change. In this study, we explore the three-dimensional structure of hillslopes and vegetation, using high-resolution airborne LiDAR (Light Detection And Ranging), to understand the long-term effects of mean annual precipitation (MAP) on catena pattern. Our results reveal that the presence and position of hillslope hydrological boundaries, or seeplines, vary as a function of MAP through its long-term influence on clay redistribution. We suggest that changes in climate will differentially alter the structure of savannas through hydrological changes to the seasonally saturated grasslands downslope of seeplines. The mechanisms underlying future woody encroachment are not simply physiological responses to elevated temperatures and CO(2) levels but also involve hydrogeomorphological processes at the hillslope scale.
Levick
Shaun R
SR
Department of Global Ecology, Carnegie Institution, 260 Panama Street, Stanford, California 94305, USA. slevick@stanford.edu
Asner
Gregory P
GP
Chadwick
Oliver A
OA
Khomo
Lesego M
LM
Rogers
Kevin H
KH
Hartshorn
Anthony S
AS
Kennedy-Bowdoin
Ty
T
Knapp
David E
DE
D000818:Animals; D002980:Climate; D017753:Ecosystem; D020049:Isoptera; D012987:Soil
D012987:Soil