Mammal diversity Final Flashcards
Gill arches
Gill arches originated in fish and are significant because they evolved from part of the jaw bone into the complex bones and structures in the modern mammalian ear. The part of the jaw that was once the gill arches broke off and divided into the malleus, cochlea, stipes, and incus that makes up modern ears.
Paedogenesis
paedogenesis, also spelled Pedogenesis, is a reproduction by sexually mature larvae, usually without fertilization. The young may be eggs, such as are produced by Miastor, a genus of gall midge flies, or other larval forms, as in the case of some flukes.
Cope’s rule
The trend towards increasing body size of members of a lineage over its evolutionary development.
Vertebrate timeline
amphibians: 370mya
reptile: 300mya
mammals: 220-240mya
dinosaurs: 220mya
birds: 150mya
homeothermy vs. poikilothermy
homeotherm: An animal that maintains a constant internal body temperature, usually within a narrow range of temperatures. poikilotherm: An animal that varies its internal body temperature within a wide range of temperatures, usually as a result of variation in the environmental temperature.
ecological shifts in mammalian selection pressures
- enhanced vision in dim light
- tactile
- smell/olfactory
- electro-receptors
- adapt to somewhat cooler temperatures at night
homodont vs. heterodont
Homodont - Teeth are all about the same shape (most vertebrates, few mammals).
Heterodont - Teeth have different forms and functions in different parts of the tooth row
diphyodont
A diphyodont is any animal with two successive sets of teeth, initially the deciduous set and consecutively the permanent set. Most mammals are diphyodonts
endothermic furnace
A 10-fold increase in metabolism, cellular mitochondria, specialized enzymes, advanced circulatory system, biconcave/eneuclate/elastic RBCs, countercurrent systems, advanced respiratory system (diaphragm and lung separation), and secondary palate allowed for eating and breathing simultaneously.
jawless fish
- round mouths
- full set of gill arches
- forward-most gill arches evolved into early jaws and pieces of the early jaw bone evolved into the bones of the ears in mammals.
mammal infraorders
marsupials, placentals, and monotremes.
Cretaceous extinction (66mya)
killed half of the world’s species, and many mammals, birds, and small reptiles survived. all dinosaurs and large reptiles perished.
Eocene (55mya)
global warming trends, Mid-Eocene sauna, increased tectonic activity near Greenland and Norway, tropical and subtropical forests spread towards the poles, increase diversity in land vertebrates, peak amphibian and reptile diversity 50mya, mammals diversity and increase in body size, by 55mya ago all 29 extant orders of mammals had evolved into existence.
late Eocene >34mya
Oligocene transition, the climate cools, the evolution of flowering plants, forests contract, and mammals adapt to eating seeds, fruit, nuts, and different habitats.
mammalian traits
- energetic
- thermoregulators
- high metabolic rate
- scales modified into fur
- highly divided lungs
- 4-chambered hearts
- sweat glands
- diaphragm
- RBCs: enucleate, discoid, flexible
- secondary palate
- heterodont and diphyodont
- zygomatic arches
- paired occipital condyles
- cervical and lumbar ribs lost
- fused pelvic bones
- quadrupedal
- long bones with epiphysis (growth plates) -> determinate growth
- increased sensory ability
American pronghorn
pronghorn-type horns, utilize group vigilance, and can run 100km/hour, they used to run from cheetahs, lions, pumas, bears, wild dogs, etc. but humans killed all of them.
Extinction
- end Permian: 245mya
- end cretaceous: 65mya (dinosaurs dead)
- late Pleistocene: 2.6-12,000 years ago (megafaunal mass extinction)
Drivers of glaciation
- eccentricity (oval)
- obliquity (angle)
- precession (orientation and tilt)
Permian extinction
- 252mya
- extinction of 90% of all species
~95% of marine life
~75% of terrestrial life - Permian extinction happened over the course of 100,000 years
- formation of Pangea caused increased instability
- increased volcanic activity: more methane and co2 caused climate change, loss of the ozone layer, and fires
- oceans mixing of deep anoxic, acidic, and sulfuric waters to the surface
- Pangea decreased coastline and caused the sea level to rise 100 meters, destroying shallow marine habitats.
- connection of terrestrial habitats caused mixing of biotas
evolutionary themes
- increased complexity of life forms
- increase the diversity of life and the total number of species
- increase the size and the range of sizes
- diversification and isolation
- chemical reactions, life in aqueous soup
- increase homeostasis – independence from external environment
- extinctions
causes of megafaunal extinction
- many plants died during the first cooling cycles
- megafaunal persistence until the later cycle of cooling.
- most extinction occurred in the largest species
- the extinction didn’t follow the same timeline so it wasn’t caused by climate.
- extinctions were the most prevalent where species were the most ecologically naive towards humans
Cenozoic era
- 66mya years - long enough for substantial drift in continents
- change in global and regional climates
- major changes in sea level and regional climates
- evolution and diversification of angiosperms
~flowering angiosperms originated 120mya but did not diversify until the Cenozoic.
End-Cretaceous climate
- warm
- isolated continents
- North and South waters mixing
- little latitudinal variation in temperatures
- the Americas has frequent contact with the other continents leading to more biota mixing
- mass extinction at the end of the Cretaceous: loss of 1/2 of the Earth’s species, all dinosaurs, and large reptiles.