BIO211H5 Lecture Notes - Chloroplast, Gowganda, Lightning
Document Summary
The precambrian originally designated as time before oldest known rocks (at the time, 3. 8 billion years ago), but now older rocks are known and included in the hadean. Precambrian craton formation of large cratons and earliest modern-style orogeny wopmay orogen: 2 billion years ago. Gowganda glacial deposits: ~2. 3 ga old craton: large non-deformed portions of very old continents, usually of precambrian age. Canadian shield: precambrian craton exporsed at surface high heat flow produced small, thinner continents continental accretion deep water sediments accreted to continent. Greenstone belts o: marine sediments form wedge between continental masses, weakly metamorphosed from igneous mafic and sedimentary rocks o o nested within high-grade felsic metamorphoc rocks abundant chlorite. Chert interbedded with sediments rich in iron formed in low o2 marine environments stopped forming 1. 9 ga (billion years) ago. Early life filamentous bacteria present ~3. 5 billion years ago stromatolites: structures built by cyanobacteria; 3. 5 billion years ago-present biomarkers for eukaryotic cells o steranes 2. 7 billion years old.