Geol 301 final Flashcards
(164 cards)
What is Rodinia
The Middle to Late Proterozoic supercontinent
When did Rodinia form
1.3 billion years ago
when did Rodinia break up
around ~750 mya
evidence for the break up of Rodinia
- development of passive margin strata around edges of Laurentia = formation of Pacific Ocean
- Grand Canyon rocks show deposition during the time in which Rodinia was rifting
Time range of Proterozoic Eon
2.5 billion to 542 million years ago
What happened during the proterozoic
- oxygenation of the atmosphere
- evolution of eukaryotes and multicellular organisms
What was the Snowball Earth Theory
Earth was covered (almost) completely in ice, most extensive glaciation in the geologic record
Evidence for Snowball Earth Theory
- neoproterozoic glacial deposits all over the world
- signatures of ice sheet movement
What are some signatures of ice sheet movement
- U shaped valleys
- moraines
- kettle lakes
- cirque: bowl shaped depression at the head of a glacier
- Arete: sharp ridge between glacial valleys
- horn: erosion by several glaciers around a single peak
- calving: the process of icebergs breaking off of glaciers when they flow into a large body of water
- dropstones
- striations
- unsorted sediments
When did snowball earth occur
- during the neoproterozoic
~640-710 mya - lasted about 10 million years each
cirque
bowl shaped depression at the head of a glacier
arete
sharp ridge between glacial valleys
horn
erosion by several glaciers around a single peak
calving
the process of icebergs breaking off of glaciers when they flow into a large body of water
dropstones
stones that were incorporated into a glacier/iceberg when it claves but are dropped out some distance away from the shoreline as the iceberg melts
How do you unfreeze a planet
- limited weathering led to build up of atmospheric CO2 -> no Ca to turn CO2 into calcite -> global warming
Evidence of Basal Metazoans
- body fossils
- trace fossils
- embryo fossils
- Molecular clock (DNA estimates)
- biomarkers slightly predate the ediacarian fauna (earliest multicellular life)
what were some characteristics of early multicellular animals
- sessile lifestyle
- multicellular complexes
- few cell types
- lack variation in tissue or organs
What can sponges tell us about the evolution of multicellularity in the late Proterozoic
a dramatic diversification of animals occurred rapidly
Evidence for sea level rise in the Cambrian
Carbonates above a transgressive sandstone, suggest transgression and marine flooding of NA
what is the Cambrian explosion
“Evolutionary experimentation”
- sudden and expansive diversification of animals
- sudden appearance of hard parts
- rapid evolution of skeletonization and new body plans
what were the Tommotian Fauna
- small (mm) shells that span the Precambrian - Cambrian transition
- the first major appearance of skeletal material
- shells from numerous groups. Many named for their shape (“from taxa”)
- tiny carbonate and phosphate shells
Age of the Tommotian Fauna
~540-528 mya
what is the significance of the tommotian fauna
the first appearance of mineralized taxa = brachiopods, trilobites, archaeocyathids, molluscs, echinoderms