Topic 11 Flashcards
evolution
gradual adaptive change over geological time, in composition of populations from ancestral species to new species
-changes to DNA through mutations occur over long time period-introduce new alleles-changing genotypic frequency-changing phenotypic frequency
microevolution
small scale changes within a gene pool of population of species over time
macroevolution
large scale changes involving species over time- new species evolves
relative dating technique
- process depends on stratification- formation of sedimentary layers of rock
- principle of superposition- older layer rocks are at bottom of strata sequence -overlain by younger layers
- gives relative age
stratigraphy
relative age of fossil is determined by position of stratum
principle of correlation
- index fossils-fossils of species existed during limited periods of geological time and found in restricted depth of strata- used as guides to age of rocks in which they are preserved
- presence of index fossil in different regions will be deemed to be same age
characteristics of index fossils
abundant, distinct, geographically widespread, found in many rock kinds, narrow in strata range
absolute dating technique
radiometric dating is a technique in which actual age of fossils and rocks is expressed in years
-radioactive decay of some elements- used to establish absolute age of fossils and rocks
potassium-argon dating
- potassium 40 decays into argon 40
- has long half life- can be used to date rocks and fossils that are over 3 billion years old
carbon dating
- fossils that contain organic matter, and are no older than 60,000 years old- can be dated using radioactive carbon dating
- carbon-14 decomposes after death due to radioactive decay
- longer since dead- lower ratio of carbon 14 to carbon 12
fossil record
-fossils provide evidence of organisms that once lived on this planet
physical fossils
- remains or whole of part of structures of organisms
- organic material of these structures is replaced by mineral or organic matter has disappeared and organism simply exists as impression
- decomposition happens quickly after death
- decomposers and scavengers get rid of soft tissue’
- weathering gets rid of bones
fossilisation
process of preserving whole or part of organism, which lived in the past
trace fossils
-preserved evidence of activities of organism, such as footprints, tooth marks, tracks, burrows and coprolites- fossilised dung
biosignatures
physical or chemical sign preserved in minerals, rocks or sediments that can be inferred to be cellular or to have resulted from organisms metabolic activity