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)