Geol 301 final Flashcards
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
What are some typical types of Cambrian fossils
- Trilobites
- inarticulate brachiopods
- echinoderms
- monoplacophoran mollusks
- stromatolites
What were Cambrian invertebrates like in terms of relative diversity and the phyla that were present compared to modern organisms?
- many different body plans
- bizarre classes of familiar phyla (each had a few species and genera)
- early echinoderms, likely related to crinoids
what is the significance of the Burgess Shale Fauna
- deep water setting with organic, low O2 sediments
- preserved soft bodied organisms (Pikaia, Onychophorans)
What is the significance of the Chengjiang fauna
- preservation of soft-bodied creatures (Corals, predatory worms, soft-bodied arthropods, anomalocarids)
What are Stromatolites
- finely laminated cyanobacterial mats that secrete calcite and climb to stay on top
What are Thrombolites
- non-layered, clotted/clustered sedimentary formations generated by cyanobacteria
Baltica
Northern Europe
Laurentia
North America
Gondwanaland
South America, Africa, Arabia, India, Australia, and Antarctica
What is the significance of stromatolites and thrombolites
- contain microbes from 500mya
- help with understanding origin and evolution of life
Archeocyathids
- early Cambrian reefs
- suspension feeders
- probably sponges
- built large reefs during early cambrian, extinct by middle cambrian
- cemented by cyanobacterial mats and other organisms that secreted calcite
What were some of the first chordate (early fish) ancestors in the cambrian
conodont (just found teeth fossils at first)
What was the Taconic Orogeny
- mountain building event that lead to the building of mountains along the north east
- Laurentia collided with a volcanic island arc, then Baltica
what caused the Taconic Orogeny
collision of ancestral North American plate with island arc (accretionary wedge crunch upward)
What is a foreland basin
- the downwarping of lithosphere behind an actively forming mountain chain
How does a foreland basin form
Subduction of oceanic crust under continental crust, magma pushes up through cc by subduction zone, cc warps up where magma is and down inland,
What is a molasse
terrestrial (river deposited) gravels and coarse sands representing collision orogenic clastics
what is a flysch
a coarsening upward sequence of sedimentary rocks that form in a foreland basin during an orogeny. Deeper water shales and shelf deposits are overlain by shoreline and terrestrial sediments as the basin fills with sediments
What are ophiolites
the remnants of very metamorphosed seafloor pinched up along suture
What factors drove diversification in the Ordovician
- high sea level and large epicontinental seas during much of the Ordovician
- restricted land, archipelagos (island chains) create a lot of shallow marine environments
- intense magmatic and tectonic activity
- strong climatic zonation = biogeographic differentiation
- asteroid bombardment
What is ecological tiering
- organisms growing taller and burrowing deeper
- diversification and specialization to meet feeding needs
What were the primary reef builders in the Ordovician
- coral-strome reefs
- tabulate corals
- stromatoporoid
- rugose corals
What were stromatoporoids
calcified sponges
What is thought to be the primary cause of the Ordovician Mass Extinction (2nd largest)
- ice age
- global cooling
- sea level drop
Main types of species affected by the Ordovician Mass Extinction
warm adapted taxa
What were the primary reef builders during the Silurian-Devonian
- coral-strome reefs
What were the dominant invertebrate predators during the Silurian-Devonian
Eurypterids and ammonoids
What were the early fish like in the Ordovician
- jawless
- boney armor
- bottom dwellers
What type of animal were conodonts
primitive craniates
- modern lamprey
when did jawed fish evolve
Evolved in the latest Silurian to Early Devonian
What were some of the major groups of jawed fish
- acanthodians (small)
- sharks
- ray finned fish
- placoderms
How did jaws evolve in fish
Food filters were modified to form gills, first gill arch became upper and lower jaws, second-gill arch moved forward to brace jaws
From what body part did fish jaws evolve
skeletal rods
when did terrestrial plants first appear
Silurian
when did amphibians first appear
Devonian
What type of plants were the first plants
non-vascular plants (mosses, liverworts, hornworts)
- spore-bearing
How do spore plants (the first plants) reproduce
by releasing spores, or small cells, that germinate
What were some of the first vascular plants
- cooksonia
- rhynia
How did vascular plants reproduce
- seeds!
what type of plants were the lycopods
- non vascular
- club mosses
- their forests formed many early coal swamps
when did seed plants evolve
Devonian