Disparity in Tree Species Richness among Biomes 43
Because different explanations for the latitudi-
nal diversity gradient may be valid for different
kinds of organisms, some have recommended that
w ec eas etrying to find a univ ersal caus e(Gas-
ton 2000). W ear esympath etic to this vi ew. For
example, the mechanisms causing the famous
reverse latitudinal gradients, such as in salaman-
d ers, ar eunlik ely to b eth esam eas th em echanism
causing forward latitudinal gradients (Williget al.
2003). But it also seems appropriate to consider
that organisms like trees take on a greater impor-
tanc eb ecaus eof th eir rol ein providing habitat,
food, and shelter for so many other organisms
(e.g., Huston’s 1994 structural versus interstitial
organisms). If w eund erstand th emost impor-
tant causes of global diversity gradients in trees,
we will also understand one element controlling
gradients of organisms that are dependent on
them for survival, such as specialist herbivorous
insects, which may represent most of the world’s
biodiversity.
Human activity is currently causing both mas-
siv eloss es of habitat and rapid climat echang e
(Corlett and Primack Chapter 26, this volume,
Laurance Chapter 27, this volume). Understand-
ing the consequences of fluctuations of biome
area through time on global tree diversity is crit-
ical as we strive to develop effective conservation
strategies. If we consider conservation of natural
habitats at the largest scales, the results reported
here suggest that tropical areas should be more
s ensitiv eto habitat loss than high-latitud ear eas
b ecaus e extinctions during th elast glacial p eriod
have likely set temperate and boreal biomes well
below their equilibrium diversity values. For this
reason, we might predict a lower extinction rate in
temperate or boreal biomes with moderate losses
in eff ectiv ear ea, whil eth esam eamount of habi-
tat d estruction in th etropics should caus emuch
higher extinction rates. Thus, because of their
greater potential for higher extinction rates, areas
in tropical biomes should be given the highest
priority for conservation.
ACKNOWLEDGMENTS
We are grateful to R. Condit, E. Dinerstein, R.
Foster, P. Grogan, C. Hawkins, H. Helmisaari,
H. Hytteborne, J. LaFrankie, R. Leemans, S. Linder,
W. Pruitt, A. Solomon, A. Svidenko, and
W. Wettengel for responding to our queries relat-
ing to information on the world’s biomes and tree
diversity estimates. We thank S. Schnitzer, C. Dick,
Z. Miller and one anonymous reviewer for help-
ful comments regarding the manuscript, and the
Michigan Society of Fellows for support.
REFERENCES
Adams, J.M. and Woodward, F.I. (1989) Patterns in tree
species richness as a test of the glacial extinction
hypothesis.Nature339, 699–701.
Baldwin, B.G. and Sanderson, M.J. (1998) Age and
rat eof div ersification of th eHawaiian silv er-
sword alliance.Proceedings of the National Academy
of Sciences of the United States of America 95,
9402–9406.
Bates, J.M., Hackett, S.J., and Goerck, J.M. (1999) High
levels of mitochondrial DNA differentiation in two
lineages of antbirds (DrymophilaandHypocnemis).
Auk116, 1093–1106.
Beerling, D.J. and Woodward, F.I. (2001)Vegetation and
the Terrestrial Carbon Cycle: Modeling the First 400
Million Years. Cambridge University Press, Cambridge.
Brown, W.L. Jr. (1957) Centrifugal speciation.Quarterly
Review of Biology32, 247–277.
Bush, M.B. (1994) Amazonian speciation: a necessarily
complex model.Journal of Biogeography21, 5–17.
Chown, S.L. (1997) Speciation and rarity: separat-
ing cause from consequence. In W.E. Kunin and
K.J. Gaston (eds),The Biology of Rarity. Chapman &
Hall, London, pp. 91–109.
Chown, S.L. and Gaston, K.J. (2000) Areas, cradles, and
museums: the latitudinal gradient in species richness.
Trends in Ecology and Evolution15, 311–315.
Crane, P.R. and Lidgard, S. (1990) Angiosperm diversi-
fication and paleolatitudinal gradients in Cretaceous
floristic diversity.Science246, 675–678.
Currie, D.J. and Paquin V. (1987) Large-scale biogeo-
graphical patterns of species richness of trees.Nature
329, 326–327.
Dowsett, H.J., Barron, J.A., Poore, R.Z.et al. (1999)
Middle Pliocene paleoenvironmental reconstruction:
PRISM2. US Geological Survey Open File Report
99–535.
Fine, P.V.A. (2001) An evaluation of the geographic
area hypothesis using the latitudinal gradient in North
American tree diversity.Evolutionary Ecology Research
3, 413–428.