history of biodiversity Flashcards
lecture 4 - John Spicer
precambian
’ before life ‘
period of time extending from about 4.6 billion years ago ( the point at which earth began to form )
age of earth
4.5 bya ( billion years ago )
earliest living organisms
Carbonacous chert clast
3465 mya
apex filament microfossils present in altered hydrothermal vent deposit
5 taxa - photosynthesises and methane producers
ealiest animal
’ worm ‘ 550 mya
ancient steriods indicate it is an animal
garden of Ediacara
earliest animals
- strange shapes sheet/leaf like
- soft bodies
- ( most ) no mouth or gut. must contain photsynthetic algae
- adapted to low oxygen levels? ( 7% - 10% of present day )
garden of ediacara : views ( earliest animals )
tradititonal view : ancestors of present day animals
Seilacher’s view : early failed experiment , no descendents
cambrian explosion
- 550 mya sudden apperaence of all major groups
- first animals with hard parts
- all major phyla ( excepy velvet worms )
why diversification now ?
- continents breaking up ( increased area of continental shelf - apperance of shallow sea - new habitats )
- climate ( much warmer than today ? critical oxygen level ? )
- developmental genetic and origin of major phyla ( development or mutation of single Hox gene - huge morphological change. mechanisms for initial rapid eveolution of body parts )
Burgess Shale fauna
discovered - Walcott 1910s
‘ rediscovered ‘ - Whittington 1960s
- typical of cambrian faunas
- many soft bodied forms
most commom species triolbite marrella
(dominant group now and then = arthropods?)
Cambrian (Cm) - pattern
start: huge radiation major groups appear
end: stabilization of many of new groups
- little ecological stabilization
(about 542 mya - 490 mya)
- paleozoic
Cambrian (Cm) - events
apperance of all major groups including jawless fish and marine ‘plants’ (algae)
Ordovician (O) - Permian (P) - pattern
Ordovician (O) - Silurian (S) - Devonian (D) - Carboniferous (C) - Permian (P)
huge increase in biodiversity. then stable for 1/4 billion years. little ecological specilisation in the sea
( about 490 mya - 300 mya )
- paleozoic
Ordovician (O) - Permian (P) - events
Ordovician (O)
- apperance of jawed fish ( cartilaginous and bony )
Silurian (S)
- first land plants
Devonian (D)
- ‘age of fish’ first amphibians. earliest insects
Carboniferous (C)
- huge terrestrial forests dominate. first reptiles
Permian (P) - pattern
ended with largest biodiversity crash known. end of paleozoic ‘early life’
(about 300 mya - 250 mya )
- paleozoic
Permian (P) - events
apperance of mammal-like reptiles
extinction of trilobites (group of arthropods)
Triassic (T) - Cretaceous (K) - pattern
Triassic (T) - Jurassic (J) - Cretaceous (K)
started with largest biodiversity crash known. begininng of mesozoic (‘middle life’). rebirth of marine biodiversity but with very different forms that increase (with blips) to prsent day
(about 250 mya to 65 mya)
*mesozoic
Triassic (T) - Cretaceous (K) - events
Triassic (T)
- marine : expansion of shell breaking predators + distruptive sediment movers. beginning of the ‘rule’ of marine mammals
- terrestrial : beginning of the rule of reptails ( + dinos )
Jurassic (J)
- age of ruling reptiles
Cretaceous (K)
- extinction of ichthyosaurs, plesiosaurs, mesosaurs and ammonites
- extinction of dinos and flying reptiles
Paleogene (Pg) - Quaternary (Q) - pattern
Paleogene (Pg) - Neogene (N) - Quaternary (Q)
beginning of the 3rd era - the cenozoic. Biodiversity continues to increse exponentially (with small blips)
(about 65 mya to now)
*cenozoic
Paleogene (Pg) - Quaternary (Q) - events
Paleogene (Pg)
- beginning of the age of mammals and flowering plants (angiosperms) on land
Neogene (N) and Quaternary (Q)
- age of insects, molluscs, fish (again) and one particular mammal
(Antropocene (A) an age of human influence and unprecedented biodiversity decline)
mass extinctions
5 big ones
end ordovician, late denovian, end paleozoic, end triasssic, K-T
background extinction rate
the number of species that would be expected to go extinct over a period of time, based on non-anthropogenic factors
(account for 96% of all extincrions over the past 600 mya)