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macroevolution
study of evolutionary processes and patterns among species
interested in the rise and fall of biodiversity (what causes it)
helps determine the origination of the tree of life: curious about where organisms evolved and from which ancestors they evolved from.
interested in how traits evolve over long time scales
showcases the rates and patterns of phenotypic evolution across time
Rise in biodiversity
periods in evolutionary history where new life forms evolved
Fall of biodiversity
periods in evolutionary history where species die off faster than new ones evolved (extinction)
proof of macroevolutionary insights
Paleontology
Phylogenetics
Paleontology
provides a direct record of past evolutionary change
inference is strong for organisms that fossilize well (can inference their history or their past life)
able to directly determine when certain organisms lived and where
provides record of how evolutionary processes came to be over millions of years
not guessing where or when an organism might have lived but fossils found in specific areas give proof of their lifestyle
Phylogenetics
indirect record of past evolutionary change
inference is the strongest for groups that have living representatives
cant inference the evolutionary history of completely extinct organisms only based on phylogenetics
can analyze the structure of phylogenetic trees to learn about the past and how species diverged as well as when
able to know the ancestors of already living species
good for obtaining information on organisms that do not fossilize we;; such as soft organisms
rich with information about the relationship between organisms and knowing when past events happened
How do phylogenetics reconstruct the history of life using evidence from organisms alive today?
use phylogenetics to find patterns used in extant organisms as an inference the behaviours of extinct organisms (shared inherited features signal shared ancestry)
How old is the earth
over 4.5 billion years old
when did life evolve
about 3.5-4.1 billion years ago with the earliest evidence of a living organism being fossilized bacteria which helped determine earth's age
when did photosynthesis evolve
about 3.2-3.5 billion years ago
when did complex cells evolve
cells that have organelles evolved by endosymbiosis about 1.8-2.2 billion years ago
symbiosis was likely between bacteria and archaea
sexual reproduction of single celled organisms evolved right after
when did multicellular life evolve
around 1.7 billion years ago
when did complex animal life grow
Complex animal life grew greatly and rapidly around 540 million years ago
this started the Cambrian explosion and marked the start of the Cambrian period
biodiversity increased greatly
when did land plants evolve
Land plants evolved around 470 million years ago
dramatically transformed the terrestrial region
Cambrian explosion
when the diversity of animals picked up the pace and similar forms to today started to diverge
started 540 million years ago
animal diversity increase dramatically over 20-30 million years (short time with context to evolution)
Found the first fossil appearance for most living animal phyla around this time
First appearance of diverse body plans like skeletons, sensory organs, predation etc.
Started gaining defensive strategies and predatory animals
Origins of cambrian explosion is still unknown but their was probably some environmental change and opportinitues for life to take advantage of
Phanerozoic eon
expands from around 540 million years ago to present
when complex multicellular life became diverse
a lot of fossils were found dating to around this time
represents 10% of earths history
90% of life on earth was single celled
biodiversity dramatically increased
Clades grouped into 3 major faunas during the Phanerozoic era
grouped by how successful they were during these times
cambrian
palaeozoic
modern
Cambrian fauna
organisms were the most diverse and successful following the Cambrian explosion
following the Cambrian era the organisms died off and were replaced. They are no longer alive today
diversity decreased
Paleozoic fauna
dominayed the planet for 200 million years
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