History of life Flashcards
indirect methods of dating
- relative dating
- paleomagnetic dating
- fauna compositions
- dendrochronological
direct methods of dating
- radiometric dating ( absolute method)
- based on the tempo of radioactive decay
- ratio of different isotopes
relative dating
using the rock layers below and above fossils as an indication of age
paleomagnetic dating
magnetic components in rock are arranged in a certain orientation due to earths magnetic piles, tempo at which poles change can be compared with the orientation
fauna composition
fossils found in between layers of volcanic rock
dendrochronological
age of trees can be determined by its annual tongs which can be used to make deductions about what happened in its past including climate conditions
archaea bacteria
the most primitive form of life, unicellular prokaryotic (no nucleus)
habitat archaea bacteria are found in
- hot volcanic areas
- warm water spouts in deep sea
- areas of little/no oxygen
- high salinity water
eubacteria
developed from archaea bacteria
lynn margulis
-developed the theory of origin
-archaea bacteria hijacked the eubacteria
-eubacteria became part of cell becoming the mitochondria providing energy while getting food and shelter from the hijacker
parasitic relationship
a single cell organism resides within another cell
endosymbiosis
A symbiotic relationship where one organism lives inside the other
fossils
- remains of organisms that lived previously and were conserved, did not decompose and their whole/parts of remained intact
how are fossils formed
- organism dies where it can be covered with sediment
- anaerobic conditions prevent decomposition
- quickly covered with sediment
- hard body parts are slowly replaced by minerals
- or the body dissolved leaving only an impression of the natural form
- cavity of mould can be filled with minerals
- whole organisms can be kept intact eg amber
body fossils
fossilisation of whole organisms or body part