1/23
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai | Chat |
|---|
No analytics yet
Send a link to your students to track their progress
When did the paleozoic era begin
542 Ma
Which of the following is not consistent with shallow-water carbonate sediment production
Areas of high river input
because of early/rapid cementation and coral reef growth on the edges of carbonate platforms, they are characteristically _____
steep-sided
the mineralogy of shallow-water carbonates does not include _____
Feldspar
what is the common requirenment for each of these prevalent, shallow-water carbonate-producing organisms: Hermatypic corals, coralline red algae, calcareous green algae, benthic foraminifera with algal symbionts
require sunlight
which shallow-water carbonate allochem (grain type) is formed through inorganic precipitation in shallow, agitated waters, and is characterized by a concentrically-layered nucleus
Ooids
In taking advantage of the warmer, stronger portions of ocean gyres, shallow-water coral reefs are largely found on the ____ side of ocean basins
western
At pulley ridge, how does the marine geology support the marine biology (coral reef ecosystem)
Provides hard substrate for coral larval attachment
in which terrigenous shelf environment, below storm wave base, are sandy storm layers (tempestites) sometimes found within an otherwise muddy deposit
offshore
Which zone of the continental shelf is characterized by sands with a distinguishing bedding pattern called hummocky cross stratification
offshore transition
what are the dominant sediment contributors to continental shelves
biogenous and terrigenous
Across continental shelves, what is the characteristic trend in grain size when going from the foreshore to the offshore
coarse to fine
which authigenic sediment formed on continental shelves is consistent with upwelling of nutrient-rich waters
phosphorite
in which type of sediments does grain size primarily reflect energy levels
siliciclastic
The majority of continental shelves are _____
wave-dominated; depths rarely exceed 10 meters
Graded beds of sand, silt, and mud deposited at the base of the continental slope by turbidity currents are called
turbidities
submarine canyons on continental shelves are the result of turbidity currents
false
which of the following two characteristics together best describe the environment of deep-sea sediment deposition
fine grained and slow accumulation
from the analysis of fine-grained mineral assemblages (such as kaolinite and chlorite), this terrestrial deep sea sediment type can be useful in reconstructing past climate/weathering signals
red clays
the solubility of ____ shells decrease with increasing pressure and decreasing temperature in the ocean. Therefore the presence of these sediments in deep sea cores indicates ______ in surface waters
silica; high productivity
The CCD is _____ in the Pacific the the Atlantic due to _____ dissolved CO2
shallower; increased
which deep sea biogenic ooze type is more abundantly found on the shallower portions of ocean ridge systems
carbonate
which of the following is the slowest accumulating deep sea sediment type (few mm’s per thousand years)
red clays
which of the following is consistent with a siliceous biogenic ooze
40% diatoms