IV. Cenozoic (65 - 0 mya). The major groups of mammals had evolved in the Jurassic and Cretaceous

Preview:

Citation preview

IV. Cenozoic (65 - 0 mya)

IV. Cenozoic (65 - 0 mya)

IV. Cenozoic (65 - 0 mya)

The major groups of mammals had evolved in the Jurassic and Cretaceous.

IV. Cenozoic (65 - 0 mya)

IV. Cenozoic (65 - 0 mya)

The extinction of the dinosaurs opened many niches, but the mammals were hammered by extinctions, too.

IV. Cenozoic (65 - 0 mya)

The extinction of the dinosaurs opened many niches, but the mammals were hammered by extinctions, too. Small mammals, however, quickly radiate into most ecological niches except large predators.

IV. Cenozoic (65 - 0 mya)

In the absence of dinosaurs, the birds radiated:

Diatryma (Gastornis) in NA/Asia

seed eater?

IV. Cenozoic (65 - 0 mya)

In the absence of dinosaurs, the birds radiated:

Phorusrhacids in SA: Top Predators

IV. Cenozoic (65 - 0 mya)

In the absence of dinosaurs, the birds radiated:

Phorusrhacids in SA: Top Predators

Largest one yet, found in Argentina in Oct. 2006, probably stood over 10 feet tall.

Chiappe and Bertelli. 2006. Nature 443:929.

2.3 ft

condor

IV. Cenozoic (65 - 0 mya)

MAMMALIAN RADIATIONS:

IV. Cenozoic (65 - 0 mya)

The nature of these radiations varied on the different, separated continents

IV. Cenozoic (65 - 0 mya)

The earliest marsupials evolved in North America, but the were practically wiped out there at the K-T. They didn't recover in NA, but weathered the K-T (and ultimately dominated the fauna) in the southern supercontinent of SA, Antarctica, and Australia, eventually radiating into all ecological niches.

late Cretaceous Alphodon, a Didelphiformian (common marsupial group)

IV. Cenozoic (65 - 0 mya)

The earliest Cenozoic marsupials are in SA (Paleocene), but by the Eocene they are present in Antarctica and Australia. They begin as insectivores...

Argyrolagus (SA)

IV. Cenozoic (65 - 0 mya)

then radiate as large herbivores (in Australia, primarily)...

Diprotodon

IV. Cenozoic (65 - 0 mya)

and finally radiate as top predators.

Thylacoleo

Marsupial "Lion"

(Australia)

'cat-like'

IV. Cenozoic (65 - 0 mya)

and finally radiate as top predators.

'cat-like'

Thylacosmilus (SA and Australia)

IV. Cenozoic (65 - 0 mya)

and finally radiate as top predators.

Borhyaena (SA)

'Dog-like'

Thylacine (Australia)

IV. Cenozoic (65 - 0 mya)

In the isolation of Australia, they radiated to fill all mammalian niches:

Insectivore

Fossorial

“teddy bear” niche 45 species of terrestrial

herbivores (Wallabies and Kangaroos

Nectarivore

Honey Possum

IV. Cenozoic (65 - 0 mya)In the isolation of Australia, they radiated to fill all mammalian

niches:

Arboreal Glider Arboreal Herbivore/Frugivore

brush-tailed Possum

IV. Cenozoic (65 - 0 mya)In the isolation of Australia, they radiated to fill all mammalian

niches:

'cat-like'

Predator

Quolls (several species)

IV. Cenozoic (65 - 0 mya)In the isolation of Australia, they radiated to fill all mammalian

niches:

'dog-like'

Predator

IV. Cenozoic (65 - 0 mya)In the isolation of Australia, they radiated to fill all mammalian

niches:

Omnivore/Scavenger

Tasmanian Devil

IV. Cenozoic (65 - 0 mya)

In SA, in addition to the marsupials, there were placental mammals - but only radiating as large herbivores:

Toxodon

IV. Cenozoic (65 - 0 mya)

and a notable mammalian clade, the Xenarthans - Sloths, Armadillos, Anteaters - were diverse and abundant in SA faunas:

Megatherium

Glyptodon

Xenarthans – a very primitive mammalian clade

IV. Cenozoic (65 - 0 mya)

and an Africarabian fauna evolved in isolation on Africa/Arabia - the modern group called that Afrotheria:

Aardvarks

Tenrecs

Hyraxes

Elephants

Elephant Shrews

Golden Moles

Is the Afrotheria polyphyletic?(1995)

Kriegs JO, Churakov G, Kiefmann M, Jordan U, Brosius J, et al. (2006) Retroposed elements as archives for the evolutionary history of placental mammals. PLoS Biol4(4): e91.

A more recent genetic analysis says no… (2006)

Curiously, this places the Pangolins (Pholidota) with Carnivores.

IV. Cenozoic (65 - 0 mya)

- Paleocene (65-55 mya)

The multituberculates dominated the "rodent niche" in northern continents. Ptilodus

IV. Cenozoic (65 - 0 mya)

- Paleocene (65-55 mya)

The first large herbivores were Pantodonts... including Titanoides and Coryphodon. There are few direct adaptations to an herbivorous lifestyle

Ptilodus

IV. Cenozoic (65 - 0 mya)

- Paleocene (65-55 mya)

The next clade of mammals were the Condylarths – omnivorous ancestral to the modern ungulates (Artiodactyls and Perissiodactlys).

Phenocodus

IV. Cenozoic (65 - 0 mya)

- Eocene (54-38 mya)

Many modern groups evolve in the northern continents:

Artiodactyls and Perrissiodactyls replace condylarths

proto- horses (Hyracotherium), tapirs, rhinoceroses, and camels, and bats, primates (Purgatorius), and whales (Basilosaurus) evolve.

Mesonychid (a condylarth)

Ambulocetus

Pakicetus

Basilosaurus

IV. Cenozoic (65 - 0 mya)

- Eocene (54-38 mya)

Icaronycterus index

IV. Cenozoic (65 - 0 mya)

- Eocene (54-38 mya)

First Primates - Plesiadapids

(Paleocene)

Purgatorius

IV. Cenozoic (65 - 0 mya)

- Eocene (54-38 mya)

Many modern groups evolve in the northern continents:

creodonts replaced large birds as major predators

IV. Cenozoic (65 - 0 mya)

- Oligocene (38-24 mya)

a cooling period, creating savannahs - grazers and browsers radiate

Mesohippus

Calicotherium

grasses evolve

IV. Cenozoic (65 - 0 mya)

- Oligocene (38-24 mya)

a cooling period, creating savannahs - grazers and browsers radiate

Arsinotherium

IV. Cenozoic (65 - 0 mya)

- Oligocene (38-24 mya)

IV. Cenozoic (65 - 0 mya)

- Oligocene (38-24 mya)

a cooling period, creating savannahs - browsers radiate

Indricotherium (Baluchitherium)

IV. Cenozoic (65 - 0 mya)

- Oligocene (38-24 mya)

Titanotheres

IV. Cenozoic (65 - 0 mya)

- Miocene (24 - 5 mya) – “NEOGENE”

IV. Cenozoic (65 - 0 mya)

- Miocene (24-5 mya)

Extensification of grassland habitats

Radiation of grazer fauna: camelids, horse ancestors, cervids, rhinos

IV. Cenozoic (65 - 0 mya)

- Miocene (24 - 5 mya)

True Dog and Cat Carnivores replace creodonts

IV. Cenozoic (65 - 0 mya)

- Pliocene (5 - 2 mya)

IV. Cenozoic (65 - 0 mya)

- Pliocene (5 - 2 mya)

Sloths, Armadillos, Porcupines, Opposum

Deer, horses, monkeys, cats and dogs, rodents

Great American Interfaunal Exchange

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

American Mastodon Mammut americanum

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

Complete Mitochondrial Genome and Phylogeny of Pleistocene Mammoth Mammuthus primigeniusEvgeny I. Rogaev, et al. 2006. PLoS.

Hyrax

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K) - Periodic Ice Ages

391.06 (2010)

379.1 (2005)

Last Maximum ~ 18,000 ybp

IV. Cenozoic (65 - 0 mya)

- Pleistocene (2 mya - 10K)

Extinction of the Pleistocene Megafuana

- Human overhunting and keystone effects

- Climate change

- diseases brought by humans and their dogs.

Recommended