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Transcript
Zoogeography of Fishes
Patterns and processes in the distribution of fishes
(i.e., what causes certain fish species to be where
they are?)
– Global
– Regional
– Local
Successively smaller sieves that determine fish
distribution
Predictability of fish assemblages
Global
Plate tectonics
Rearrangement of
land masses
– sunfishes restricted to
N.A. (arose following
split of land masses,
temperate, freshwater)
Regional - Historic
Drainage Divides
– Broad drainages
isolate aquatic
communities
(Mississippi vs
Atlantic Slope)
Regional - Historic
Drainage Divides
– Drainage
rearrangement (stream
capture)
– Populations of
Mississippi R. fishes on
Atlantic slope
– Etheostoma
blennioides (Potomac
captured Mississippi)
Regional—Historic
Glaciation
– Mississippi Drainage oriented N – S
Fish disperse south
– Atlantic Drainage oriented E – W
– Teays R was the major N-W flowing river
Ice sheets dams caused it to flow S through the
small Mississippi R.
Melt water cut through central highlands making
Mississippi R the major river
– Ancient Teays River Valley near present-day
New and Kanawha Rivers
Pre-Pleistocene
Pleistocene
SE Fish Richness
•Tennessee
River most
diverse
•Atlantic slope
least diverse
•New /
Kanawha
River basin
“relatively
diverse”
Warren et al. 1997
Regional - Local
Geology (regional characteristic that
influences local conditions)
– Habitat
– Water Flow
– Chemistry
Alkalinity - Hardness
Productivity
Regional - Local
Spatial Position
– The position of a stream segment in a stream
network influences species found there
(distance from a species pool).
Influence of Barriers
Influence of Stochastic Events
Local
Competition / Predation
Water Chemistry
Water Flow
Productivity
Habitat
Gradient
Stream Size
25
Species Richness = -5.16 + 4.6 x (Basin Area) + 0.39 x (Link Order Diff)
R2 = 0.79
df = 17
p < 0.0001
Observed Richness
20
15
10
5
0
0
5
10
Expected Richness
15
20