Unit 1 Flashcards
How old is life?
3.7 billion years
study of fossils
paleontology
relative position of layers and their place in geological time scale
stratigraphy
what are the layers of rock called?
strata
extant
living today
geologic time is divided into
eons, era, period, epoch
We are in what eon?
Phanerozoic
We are in what era?
Cenozoic
We are in what period?
Quaternary
We are in what epoch?
anthropocene
What is the age of homo sapiens?
200,000 years ago
What is the age of animals?
500-600 million years ago
What is the age of life/prokaryotes?
3.7 billion years ago
What is the age of Earth?
4.5 billion years ago
Fault
crack in Earth’s crust
Where have fault lines been found?
1975 earthquake in Morris
Rocks in (blank) MN are 3 bya
Montevideo
What eon are we living in?
Phanerozoic
What era are we living in?
Cenozoic
What period are we living in?
Quaternary
What epoch are we living in?
Anthropocene
How old are homo sapiens?
200,000 years old
How old is life on land?
300 million years
How old are animals?
500 to 600 million years
How old is life/prokaryotes?
3.7 billion years
How old is Earth?
4.5 billion years
What is the first step of oxygen throughout time?
1) CO2 + H2O—- Sugar + O2
Early atmosphere had little or no free O2 until photosynthesis released O2 as a waste product
List steps 2-5 of the role of oxygen throughout time
2) O2 in water + iron = BIF
3) GOE killed anaerobes; aerobes thrived (high O2 concentration supports large cells)
4) O2 increased, allowed eukaryotes and multicellular life
5) invasion of land by plants, increased O2
formation of BIF
- oxygen captured by iron in water which fell to the sea floor creating a BIF
- sedimentary in mesabe range NE MN
great oxygenation event
- water saturated with O2 was the tipping point that led to the goe
- opened resources for aerobic bacteria
development of complex life
-rise of aerobic lifestyle; efficient, led to eukaryotes and multicellularity due to the surface area to volume ratio of oxygen in larger cells (vs previous small cells) due to diffusion
invasion of land
invasion by plants led to an increased amount of O2 due to increase in photosynthetic processes
great dying
- cause unknown
- low O2
describe general carbon trends over past 400,000 years
- Plesitocene
- Petit graph (temp and CO2 data could be placed on top of each other because they are so similar, up and down until present day)
- Lake Vostok in Antarctica CO2 and temp both from ice
describe general carbon trends over past 300 years
- Keeling curve measures CO2 levels
- Hawaii steady increase, senses seasons
- fluctuating between 175 and 275 ppm until present
- present day CO2 increase past 400 ppm
- “the world passes 400 ppm carbon dioxide threshold. permanently” - Sept 2016
- –should have been at lowest point after season
How do we know these general carbon trends?
glacial formations
How are glacial formations evidence of past climate change?
new ecosystems developed after glaciers
- geologic formations
- vegetation records
What are some examples of glacial formations? When did they disappear?
end moraine, kame, esker, coteau, 10000 years ago
terminal dump of glacial debris
end moraine
hill of sand debris laid by glacial meltwater
kames
ridge of sand/debris, laid by meltwater
eskers