The antiquity of Madagascar's grasslands and the rise of C-4 grassy biomes
Document Type: Journal
Author(s): W. J. Bond ; J. A. Silander ; J. Ranaivonasy ; J. Ratsirarson
Publication Year: 2008

Cataloging Information

  • Africa
  • Africa
  • biome origin
  • birds
  • carbon
  • charcoal
  • deforestation
  • deforestation
  • distribution
  • East Africa
  • ecosystem dynamics
  • fire frequency
  • flammability
  • forest management
  • grasses
  • grassland
  • grasslands
  • histories
  • Madagascar
  • Madagascar
  • mammals
  • native species (animals)
  • native species (plants)
  • nongame birds
  • organic matter
  • paleoecology
  • pollen
  • presettlement fires
  • reptiles
  • savanna
  • savannas
  • small mammals
  • soil organic matter
  • South Africa
  • wildfires
  • wildlife habitat management
  • woody plants
  • International
Record Maintained By:
Record Last Modified: June 1, 2018
FRAMES Record Number: 48008
Tall Timbers Record Number: 24053
TTRS Location Status: In-file
TTRS Call Number: Fire File
TTRS Abstract Status: Okay, Fair use, Reproduced by permission

This bibliographic record was either created or modified by the Tall Timbers Research Station and Land Conservancy and is provided without charge to promote research and education in Fire Ecology. The E.V. Komarek Fire Ecology Database is the intellectual property of the Tall Timbers Research Station and Land Conservancy.


Aim Grasslands and savannas, which make up > 75% of Madagascar's land area, have long been viewed as anthropogenically derived after people settled on the island c. 2 ka. We investigated this hypothesis and an alternative -- that the grasslands are an insular example of the post-Miocene spread of C4 grassy biomes world-wide.Location Madagascar, southern Africa, East Africa.Methods We compared the number of C4 grass genera in Madagascar with that in southern and south-central African floras. If the grasslands are recent we would expect to find fewer species and genera in Madagascar relative to Africa and for these species and genera to have very wide distribution ranges in Madagascar. Secondly, we searched Madagascan floras for the presence of endemic plant species or genera restricted to grasslands. We also searched for evidence of a grassland specialist fauna with species endemic to Madagascar. Plant and animal species endemic to C4 grassy biomes would not be expected if these are of recent origin.Results Madagascar has c. 88 C4 grass genera, including six endemic genera. Excluding African genera with only one or two species, Madagascar has 86.6% of southern Africa's and 89.4% of south-central Africa's grass genera. C4 grass species make up c. 4% of the flora of both Madagascar and southern Africa and species : genus ratios are similar (4.3 and 5.1, respectively). Turnover of grasses along geographical gradients follows similar patterns to those in South Africa, with Andropogoneae dominating in mesic biomes and Chlorideae in semi-arid grassy biomes. At least 16 monocot genera have grassland members, many of which are endemic to Madagascar. Woody species in frequently burnt savannas include both Madagascan endemics and African species. A different woody flora, mostly endemic, occurs in less frequently burnt grasslands in the central highlands, filling a similar successional niche to montane C4 grasslands in Africa. Diverse vertebrate and invertebrate lineages have grassland specialists, including many endemic to Madagascar (e.g. termites, ants, lizards, snakes, birds and mammals). Grassland use of the extinct fauna is poorly known but carbon isotope analysis indicates that a hippo, two giant tortoises and one extinct lemur ate C4 or CAM (crassulacean acid metabolism) plants.Main conclusions The diversity of C4 grass lineages in Madagascar relative to that in Africa, and the presence of plant and animal species endemic to Madagascan grassy biomes, does not fit the view that these grasslands are anthropogenically derived. We suggest that grasslands invaded Madagascar after the late Miocene, part of the world-wide expansion of C4 grassy biomes. Madagascar provides an interesting test case for biogeographical analysis of how these novel biomes assembled, and the sources of the flora and fauna that now occupy them. A necessary part of such an analysis would be to establish the pre-settlement extent of the C4 grassy biomes. Carbon isotope analysis of soil organic matter would be a feasible method for doing this. © 2008 The Authors. Journal compilation © 2008 Blackwell Publishing Ltd. Abstract reproduced by permission.

Online Link(s):
Bond, W. J., J. A. Silander, J. Ranaivonasy, and J. Ratsirarson. 2008. The antiquity of Madagascar's grasslands and the rise of C-4 grassy biomes. Journal of Biogeography, v. 35, no. 10, p. 1743-1758. 10.1111/j.1365-2699.2008.01923.x.