Lecture 4- Marine Geology Flashcards
origin of life on earth- 4 billion years ago
first life on earth (ocean only)
origin of life on earth- 3 billion years ago
oxygen atmosphere formed from the actions of bacterial photosynthesis in the ocean
origin of life on earth- 550 million years ago
- Cambrian explosion
- first life on land
origin of life on earth- 250 million years ago
- largest mass extinction
- first mammals and dinosaurs
origin of life on earth- 65 million years ago
- asteroid impact
- end of dinosaurs, rise of mammals
How many mass extinctions have there been?
5
bathymetry
measurement of depth of water in oceans, seas, or lakes
SONAR
sound navigation and ranging
single beam sonar
creates TRACKLINE of bottom depth
towed multi beam sonar
creates a HIGH RESOLUTION SWATH of the bottom depth
multi beam sonar
creates SWATH of bottom depth
Theory of Continental Drift (1915)
- proposed by Alfred Wegener
- was not well accepted because the forcing mechanism he proposed was wrong (tidal action of the moon)
Plate Tectonic Thoery
accepted after “sea floor spreading” and “sea floor subduction” were discovered (correct forcing mechanisms)
Earth’s composition: rigid outer crust
- thin and rigid
- floats on the mantle
Earth’s composition: plastic upper mantle
- solid
- high temperatures cause the material to be ductile enough to flow on very long timescales
paleobiography
Wegener noted that in addition to the apparent good fit of the continents, the fossil and mineral distribution made sense if the continents were joined together in the past
mid-ocean ridges
discovered with WWII sonar
magnetic anomaly
- proxy of geologic time, each anomaly can be assigned to a specific date
- provided strong evidence of seafloor spreading
earth’s magnetic field
- is not that stable
- has gone many reversals over time
paleomagnetism
strips of alternating magnetic polarity
strong evidence that the ridge is slowly spreading away from the ridge in opposite directions
rock getting older symmetrically as you move away from the ridge
deep sea trenches and associated seismic activity
helped to explain the eventual loss of ocean crust that was eventually formed at mid-ocean ridges
convection
process in which hot molten rock rises to the surface at DIVERGENT boundaries
subduction boundaries
- hot molten rock cools and become more dense at the surface
- cooled rock sinks and is pulled by gravity back into the mantle at these boundaries
origin of life on earth- 2 billion years ago
first multicellular life (ocean only)
Devonian
Age of Fishes
origin of jaws
ca 450 Ma
oldest known bone
ca 500 Ma