History of Life on Earth - Ch. 18 Flashcards
Fossil records
how scientists date and record and reconstruct history. Fossils can be found in sedimentary rock, mineralized, and organic. The fossil record is an incomplete record, this is because some organisms may not have been preserved, some destroyed, and some not found yet.
Relative dating
uses the order of rock strata to determine relative age of fossils.
Radiometric dating
measures decay of radioactive isotopes present in layers where fossils are found - uses half life, which is the amount of time it takes for 50% of the substance to decay
How many years ago was the first prokaryote present?
3.5 billion years ago
When did O2 start to accumulate in the atmosphere?
2.7 billion years ago
When were the first eukaryotes present?
2.1 billion years ago
When did the first multicellular eukaryotes appear?
1.2 billion years ago
When did plants start colonization?
500 million years ago
When did humans appear?
200,000 years ago
Endosymbiat theory
mitochondria and plastids were once individual and small prokaryotes. eventually the prokaryotes joined together with a smaller cell and worked cohesively together, eventually forming what is known today as a eukaryotes.
Evidence of endosymbiat theory
replication of binary fission, single and circular DNA, ribosomes to make proteins, enzymes similar to living prokaryotes, and two membranes
Pangea
was a super continent that formed about 750 million years ago. continental drift helps explain many bio-geographical puzzles, such as the separation of the continents. movement of the continental plates change geographically and climate of earth and caused mass extinctions.
Pre-cambrian era
microscopic fossils, development of photosynthesis and eukaryotic species (endosymbiat theory)
Paleozoic era
cambrian explosion, plants invade the land and animals start to appear. During this era the permian extinction occurs, causing 96% of species to go extinct
Mesozoic era
age of reptiles and plants and the origin of mammals, formation of pangea, there is a cretaceous extinction that occurs because of an asteroid off Mexico’s coast
Cenozoic
primates form
Evolutionary development (Evo Devo)
evolutionary developmental biology. evolution of new forms results from changes in DNA or regulation of developmental genes
Gene regulation
also called homeotic genes, and they are responsible for master regulatory genes that determine location and organization of body parts
Heterochony
evolutionary change in rate of developmental events
Hox genes
an example of homeotic genes.
a group of related genes that control the body plan of an embryo along the cranio-caudal axis (head tail axis).
After the embryonic segments have formed, the Hox proteins determine the type of segment structures (e.g. legs, antennae, and wings in fruit flies or the different types of vertebrae in humans) that will form on a given segment.
Exaptations
structures that evolve but become co-opted for another function. an example would be bird feathers = thermoregulation and flight
Speciation
the formation of two species from one original species
for speciation to occur, two new populations must form from one original population and evolve in that it becomes impossible for individuals from two populations to interbreed
Microevolution
changes in allele frequencies (different versions of a gene) within a single gene pool
Macroevolution
evolutionary change above the species level