Lecture 7 Flashcards

1
Q

Microbial Cells

A
  • first fossils of these 3.5 billion years ago and origin of earth around 4.6 billion years ago with life arising just around 4.2 billion years
  • 2.4 billion years ago, there is an oxygen spike due to cyanobacteria, not permanent and levels fall again with changes the acidity of the ocean
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2
Q

Cambrian

A
  • refers to the flowering of animal evolution

- more unstable–>competition

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3
Q

Trigger for multicellularity

A

-rise in oxygen levels

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4
Q

Precambrian ecosystems and cellular life

A
  • stable because there’s no predation
  • Eubacteria-include cyanobacteria in stromatolites
  • later fossil cells-younger than 2byr indicate Eukaryotes
  • the third great kingdom: Archaea. Primitive in many ways and specialized to strange environment and some odd metabolism
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5
Q

Snowball Earth

A
  • when earth had very big ice ages and glaciers were almost to the equator
  • after this earth starts seeing first, faint trace fossils as well as the first large Ediacara Fauna animals
  • you can see these even if you can’t see the animal itself–>something walked/burrowed here
  • oxygen level rise to roughly modern levels, and animals appear in the fossil record for the first time
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6
Q

Ediacara Fauna

A

-found all over surface of Earth

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7
Q

Bacterial mat

A
  • dominae earth from 3.5 bry 550 myr ago

- earth was this way for at least three billion years of its 4.5 byr existence

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8
Q

Cambrian radiation

A

-started 542 myr ago

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9
Q

End of Precambrian

A
  • precambrian ecosystems stable, slow evolution, saturated
  • 2 bya first good signs of eukaryotes
  • 635 mya first signs of multicellular animals
  • most striking effect on PC ecology is stromatolites. Old stability gone by start of the Cambrian. Increased competition, unsaturated world, dynamic
  • due to direct grazing of microbial films by animals
  • rise on free oxygen
  • change in 12C/13C ratios in buried organic carbon
  • heterotrophs were eating photosynthetic carbon and it was buried rapidly in fecal pellets
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10
Q

Ediacara Fauna

A
  • body fossils of elaborate large creatures that potentially are ancestral animals.
  • unusual enough to require critical evaluation
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11
Q

Small shelly fossils

A

-tiny simple tubes at first with later increase in diversity

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12
Q

Order of origin life

A
  • sponges come first, then rest of metazoans
  • edicara fauna and trace fossils
  • burrows (start of cambrian)
  • small shelly fossils
  • skeletons
  • arthropods
  • burgess shale like faunas
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13
Q

Precambrian thing and yellow (seapen)

A
  • analog has been made many times in appearance of body orientation
  • can’t tell if Precambrian one has polyps like yellow guy
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14
Q

Spirgiania

A

-related to living arthropods? can it move? oriented vertically and acts as fan in sediment?

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15
Q

Kimberella

A

-seemed to have covering on top and fed by crawling on the sea floor

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16
Q

What were edicara animals?

A
  • vendazoans, not animals at all fungal grade
  • extinct group of creatures related to animals
  • odd cnidarian and ctenophore radiation
  • primitive memebers of living phyla and ancestors to living phyla
  • new data supports 3 and 4 even with a creature that is likely an ancestral bilaterian (Kimberella)
17
Q

The metazoan radiation and origins of the phyla

A
  • timing
  • problem of interpreting fossils of very long ago animals
  • origins of body plans=phyla? old ones still extant?
  • phylogenetic relationships to each other and to living animals
  • rates and mechanisms
18
Q

Diploblast

A

-two body layers: ectoderm and endoderm

19
Q

Triploblast

A
  • three germ layers: ectoderms, mesoderm, endoderm

- bilateral symmetry

20
Q

Celomic

A
  • body cavity

- innovation that is a sac that contains all the organs outside the gut

21
Q

Body plans

A

-different body plans evolve independently because heart and nerve cord can be on either side

22
Q

Metazoa

A
  • 35 phyla
  • most primitive but no tissues or organs
  • advanced animals: eumetazoa-symmetry and tissues two groups Cnideria and Bilateria
23
Q

Cnideria

A
  • radial symmetry
  • tissues
  • no organs
  • ctenophores of similar grade
24
Q

Bilateria

A
  • bilateral symmetry
  • complex organs
  • major actors in Cambrian radiation
25
Q

Cambrian soft-bodied faunas

A
  1. Burgess Shale, Canadian Rockies discovred by Charles Walcott
  2. Sirius Passet Greenland
  3. Chenjiang, China
    - even with invention of skeletions, most animals in sea are and were soft-bodied
    - skeleton only preserve a small part of entire living animal
26
Q

Advances in metazoan body structure

A
  • bilateral symmetry and polarity
  • three germ layers
  • complex organs
  • coelomic body cavity
  • segmentation
  • important in making possible the Cambrian Radiation
27
Q

Segmentation

A

Not all animals are segmented, but most are

  • Matamerism or segmentation
  • repeats of segments that resemble one and other as you go down the body axis
  • segmentation allows for the building of a body plan in a very economic way
  • used in annelidia, arthropoda, and chordata