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Lecture 5 Mammal Zoogeography. Triconodontidae. Multiturberculata. Spalacotheriidae. Paurodontidae. Dryolestidae. Amphilestidae. Docodontidae. Amphitheridae. Shuotherium. Sinoconodontidae. Morganucodontidae. Haramiyoidea. Phylogeny of Mesozoic Mammals. 0 Yrs. CENOZOIC. MONOTREMES.

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Lecture 5 Mammal Zoogeography

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Lecture 5 mammal zoogeography l.jpg

Lecture 5Mammal Zoogeography


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Triconodontidae

Multiturberculata

Spalacotheriidae

Paurodontidae

Dryolestidae

Amphilestidae

Docodontidae

Amphitheridae

Shuotherium

Sinoconodontidae

Morganucodontidae

Haramiyoidea

Phylogeny of Mesozoic Mammals

0 Yrs

CENOZOIC

MONOTREMES

PLACENTALS

MARSUPIALS

65 MY

‘K-T boundary’

CRETACEOUS

?

Ornithorhynchidae

?

?

145 MY

Peramuridae

JURASSIC

Kuehneotheriidae

?

215 MY

TRIASSIC

(from Carroll 1988, pp. 415)


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What is Zoogeography?

Zoogeography is the study of the geographical distributions of animals

Zoogeography seeks answers to questions like:

Why are there marsupials in Australia and South America?

Why are members of the camel family (Camelidae) found in north Africa and South America?

Why are there primates from Japan to Africa, as well as South but not North America?


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Principles of Ecological Zoogeography

Endemism

all species have a limited distribution on a world scale. Some mammals are very well dispersed - eg. Humans, their stock, and commensuals like the house mouse (Mus domesticus), whereas others have a very limited distribution.

Endemism (occurring nowhere else), or being endemic - a taxon is restricted to a limited geographical area.

Endemism depends on the scale you are referring to - it might be a small area like an island, or an entire continent.

Endemism can refer to a single species, genus, family, order, or other grouping.


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Principles of Ecological Zoogeography

Convergence

when groups of mammals become geographically isolated, they usually diverge - meaning they adapt (over a long time span) to the specific climatological, geological and ecological situation they are faced with.

However - sometimes convergence occurs - convergence occurs when distantly related lineages inhabiting regions with similar climatological, geological and ecological situations evolve similar morphologies, life history patterns or niche characteristics.

Numerous examples of convergence exist among mammals


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echidna (Tachyglossus)

pangolin (Manis)

aardwolf (Protoletes)

Giant anteater (Myrmecophaga)

aardvark (Orycteropus)

numbat (Mymecobius)


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Principles of Ecological Zoogeography

Mammals on Islands

  • Islands can be the traditional sort (surrounded by water!), or isolated mountain ranges, deserts, parches of suitable vegetation etc - “habitat islands”

  • Dispersal to islands is a problem for mammals - rodents and bats are the most successful island colonisers - eg. rodents and bats are the only terrestrial eutherians to reach Australia, and the Galapagos Islands.

  • Different selective pressure on islands vs. mainland affects some characteristics of mammals:

    • niche expansion - ‘competitive release’

    • body size - can be larger or smaller than mainland counterparts

    • behaviour - predator aviodance, etc


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Principles of Ecological Zoogeography

Latitudinal Gradients

Species diversity of mammals (and most other life forms) increases along a gradient from the poles to the Equator

  • Several theories proposed :

  • higher productivity and stability in tropics

  • greater habitat heterogeneity in tropics

  • more spp. = > competition & specialization

  • harder to adapt to colder climates

  • parasite loads > in tropics

  • Not always the case

    • seals and baleen whales reach peak diversity at high latitudes

    • Drylands in Sth America has > diversity of endemics than lowland Amazon r’forest


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Palearctic

Nearctic

Ethiopian

Oriental

Neotropical

Australian

Faunal Regions


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Plate Tectonics

Plate Tectonics - theory that the earth’s crust, including the continents and ocean floors, is made up of a series of plates, as plates collide volcanoes occur, and may result in oceanic islands, mountain ranges etc.

Continental Drift - movement over geological time of the earths large land masses as a result of plate tectonics

  • Wegener (1912, 1915) - but not accepted until 1960s


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Marsupial Zoogeography

Marsupials evolved in North America (diverse fossil evidence from southern Canada & western USA)

Dispersed south to South America, Antactica and Australia, and East to Europe & north Africa

Gondwana split from Pangaea, and marsupials underwent extensive radiation in relative isolation

Marsupials in North America and Europe went extinct, possibly due to radiation and expansion of the Eutherians

Antartica drifted south - massive extinction. Australia drifted east, enormous radiation


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Dispersal and Centres of Origin

Passive Dispersal - movements in which the dispersing organism plays no active role in the movement Eg. rafting, or being transported by humans

Active Dispersal - involves an accumulation of ecological dispersal events in which individuals move by terrestrial locomotion or flight

active long-term species dispersal movements, also called faunal interchanges, occur via several routes.

Corridor Route - minimal resistance to the passage of animals (eg. present interconnection of Asia and Europe)

Filter Route - allows only certain species to pass through - eg. Beringia. Only mammals adapted to the cold climate could successfully cross between the continents.

Sweepstake Route - most restrictive pathway. Involves movement of animals by swimming, flying, rafting or other means . Unlikely to be crossed by large numbers of a given type of animal, but occasional one will make it. Eg. New Guinea to Australia to New Zealand


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Glaciation and Refugia

During the Pleistocene several cool, dry glacial periods, interspersed with warmer and wetter interglacial periods have had a substantial effect of mammal distributions

There have been 4 glacial periods in the last 600,000 years, with the most recent one ending approx. 12,000 years ago. We are currently in an interglacial (warm, wet) period

During each glacial period, ice sheets expanded and many species were displaced, some driven to extinction. During glacial periods, however, the sea level was lower and some land bridges formed (eg. Bering land bridge)

During the interglacial periods, episodes of recolonisation and resettlement occurred, and sea level rose, isolating some species


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Glaciation and Refugia: Beringia

Beringia was a land mass which was largely ice-free during the last glacial period (90,000 - 10,000 years ago) due to its arid climate

It acted as a refugium for several mammals, as well as a land bridge for animals to cross between Eurasia and North America

(from Pringle 1999)

Land bridge was submerged again approx. 11,000 years ago (to the present)


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Beringia Mammals

Steppe bison (Bison priscus)

American lion (Panthera leo atrox)

Others included:

short-faced bears (Artodus)

mastodon (Mammut americanum)

woolly mammoth (Mammuthus primigenius)

Scimitar cat (Hometherium serum)

camels (several genera)

first humans in North America

Giant beaver

(Casteroides ohioensis)

Jefferson’s ground sloth

(Megalonyx jeffersonii)

(from Pringle 1999)


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1.8 million years ago

470,000 years ago

Mammuthus (mammoth)

Synaptomys (bog lemming)

Microtus (vole)

Ondatra (muskrat)

Microtus pennsylvanicus (meadow vole)

M. montanus (montane vole)

Cervalces (extinct stag moose)

Rangifer (caribou)

Oreamnos (mountain goat)

Ovibos (musk ox)

Ovis (sheep)

Alces (moose)

Bos (yak)

Saiga (antelope)

Bootherium (extinct bovid)

1.2 million years ago

Clethrionomys (red-backed vole)

Phenacomys (vole)

Synaptomys (bog lemming)

Microtus (vole)

Bison (Bison)

Gulo (wolverine)

Smilodon (saber-tooth cat)

70,000 years ago

Clethrionomys rutilis (red-backed vole)

Microtus oeconomus (tundra vole)

170,000 years ago

Dicrostonyx (collared lemming)

Lemmus (lemming)

Lagurus (vole)

Microtus (vole)

Beringia Immigrants


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Panamanian Land Bridge

Stopped by Filter

many bats

most armadillos

anteaters

sloths

most histricomorphs


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Panamanian Land Bridge

porcupine

nine-banded armadillo

Crossed Filter


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Panamanian Land Bridge

Stopped by Filter

shrews

kangaroo rats

pocket gophers

beavers

bobcats

pronghorn antelope

bison

sheep


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Panamanian Land Bridge

Rabbits

squirrels

mice

dogs

bears

raccoons

weasels

otters

skunks

puma

deer

Crossed Filter


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Panamanian Land Bridge

Cannot Recross Filter

coatis

kinkajous

tapirs

peccaries

camels


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Camelidae Zoogeography

Camelidae - Bactrian camels (Camelus bactrianus) and dromedaries (C. dromedarius) occur in north Africa, and llama (Lama glama), alpaca (L. pacos), guanaco (L. guanicoe) and vicuna (Vicugna vicugna) occur in South America

Camelids arose and diversified in North America, with some forms eventually dispersing across the Bering Land Bridge (Beringia) to Eurasia and Africa, and the Panamanian Land Bridge to South America

North American camelids went extinct towards the end of the last glaciation


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