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BIO 152 Test 2 Part2

Part 2 Chapter 25

QuestionAnswer
Macroevolutionary changes getting new species and new groups over large time scales (terrestrial vertebrates, photosynthesis, long-term impacts of mass extinctions)
Reducing environment one that favors the formation of chemical bonds (prehistoric)
Oxidizing environment favors the breaking up of chemical bonds (today’s environment)
A.I. Oparin and J.B.S. Haldane hypothesized that the early atmosphere was a reducing environment
Stanley Miller and Harold Urey conducted lab experiments that showed that abiotic synthesis of organic molecules in a reducing atmosphere is possible
Key properties of life replication and metabolism
Protobionts aggregates of abiotically produced molecules surrounded by a membrane or membrane-like structure; exhibit simple reproduction and metabolism and maintain an internal chemical environment; not a living organism but has many characteristics
Liposomes laboratory version of protobions
Ribozymes RNA molecules that have been found to catalyze many different reactions; can make complementary copies of short stretches of their own sequence or other short pieces or RNA
Strata layers where sedimentary rocks are deposited; richest source of fossils; reveals relative ages of fossils
Radiometric dating determines the absolute ages of fossils
Half-life the time required for half the parent isotope to decay
Tetrapods the group of animals mammals belong to
Geologic record divided into the Archaean, the Proterozoic, and the Phanerozoic eons
Phanerozoic encompasses multicellular eukaryotic life; divided into three eras 1. Paleozoic 2. Mesozoic 3. Cenozoic
Stromatolites the oldest known fossils; rock-like structures composed of many layers of bacteria and sediment; date back 3.5 billion years ago
Prokaryotes Earth’s sole inhabitants from 3.5 to 2.1 billion years ago
O2 most is of biological origin; produced by oxygenic photosynthesis reacted with dissolved iron and precipitated out to form banded iron formations; 2.7 billion years ago began accumulating in the atmosphere and rusting iron-rich terrestrial rocks
Oxygen revolution 2.7 to 2.2 billion years ago; posed a challenge for life, provided opportunity to gain energy from light; allowed organisms to exploit new ecosystems
Endosymbiosis hypothesis that proposes that mitochondria and plastids (chloroplasts and related organelles) were formerly small prokaryotes living within larger host cells)
Endosymbiont a cell that lives within a host cell
Serial endosymbiosis supposed that mitochondria evolved before plastids through a sequence of endosymbiotic events
Oldest known eukaryote fossils 2.1 billion years ago
Oldest known fossils of multicellular eukaryotes 1.2 billion years ago
Snowball Earth hypothesis suggest that periods of extreme glaciation confined life to the equatorial region or deep-sea vents from 750 to 580 million years ago
Ediacaran biota an assemblage of larger and more diverse soft-bodied organisms that lived from 565 to 535 million years ago
Cambrian explosion refers to the sudden appearance of fossils resembling modern phyla in the Cambrian period (535 to 525 million years ago); provides the first evidence of predator-prey interactions
Fungi, plants, and animals began to colonize land about 500 million years ago
Plants and fungi likely colonized land together by 420 million years ago
Arthropods and tetrapods the most widespread and diverse land animals
Tetrapods evolved from lobe-finned fishes around 365 million years ago
Permian extinction occurred in less than 5 million years and caused the extinction of about 96% of marine animal species; defines the boundary between the Paleozoic and Mesozoic eras
Cretaceous mass extinction 65.5 million years ago, separates the Mesozoic from the Cenozoic; about half of all marine species went extinct and many terrestrial plants and animals including most dinosaurs
Created by: AliRutherford
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