Chapter 25 terms and concepts Flashcards
Describe steps by which simple cells may have originated from non-living materials
- The abiotic (nonliving) synthesis of small organic molecules, such as amino acids and nitrogenous bases
- The joining of those organic molecules into macromolecules, such as proteins and nucleic acids
- The packaging of these molecules into protocells
- The origin of self-replicating molecules that eventually made inheritance possible
Protocell
An abiotic precursor of a living cell that had a membrane-like structure and maintained an internal chemistry different from its surroundings.
(Abiotically produced vesicles have even demonstrated simple reproduction and metabolism, homeostasis)
Ribozymes (and which genetic material came first, DNA or RNA)
The first genetic material was most likely RNA, not DNA. RNA is much more efficient with replication, and makes fewer errors in replication, and thus is hypothesized to precede DNA given it’s ability to create descendant molecules.
RNA plays a central role in protein synthesis, but also functions as an enzyme-like catalyst. Ribozymes are enzyme-like catalysts (ie - an intron that catalyzes its removal during RNA splicing)
Why do some scientists believe that RNA, rather than DNA, was the first genetic material?
A. RNA has both information storage and catalytic properties.
B. RNA contains uracil in place of thymine.
C. RNA could have evolved into DNA.
D. RNA can replicate more accurately than DNA.
E. All the proto-cells on early Earth contained RNA.
A
Explain what fossils are, how they are dated, and what the fossil record can reveal about life’s history
Fossils are remnants of organisms that have been preserved in (most likely) sedimentary rock
Macroevolution
Applies to major evolutionary changes, such as whole taxonomic groups over long periods. The development of large-scale structures and traits that go significantly beyond the different traits in microevolution
Microevolution
Minor evolutionary changes within a species that allow for increased fitness in a certain specific environment. These changes are due to allele frequencies that occur over time
Types of fossils (from most to least abundant)
(Most abundant)
1. Trace fossils: indirect evidence left by an organism: footprints, feces, habitats
2. Molds/casts: an impression of an organism, a cast is a mold filled with sedimentary rock.
3. Replacement: The original organic material of the organism is replaced by mineral crystals that leave replicas of the organism
4. Petrified: Empty pore spaces are filled in by minerals, such as petrified wood
5. Amber: Tree sap which is preserved traps the entire organism. Sap hardens into amber
6. Original material: mummification or freezing preserves the original organism
Why is the fossil record biased?
It only has preserved species that live for a long time, were abundant and widespread in certain environments, had hard structures that could be preserved, etc.
How are fossils dated?
Radiometric dating, which focuses on the decay of radioactive isotopes that decay at fixed rates.
C-14 half-life is 5730 years, and when the ratio is compared to the fixed C-12 isotope, you can date the fossil.
ratio is 1/16 of a fossil, then the fossil would be 5730 * 4 (for 4 half lives) = 22,920 years old
What can the fossil record tell us about life’s history?
It shows that there have been great changes in the kinds of organisms on Earth at different points in time. It also shows the age of the Earth and the organisms that have inhabited it
The clock analogy
- The origin of the solar system and Earth, followed by the Hadean period (4.6 bya)
- The Archaean period (4 bya - 2.5 bya), where prokaryotes emerged (3.5 bya). At end of archean period, atmospheric oxygen formed (~2.75 bya) due to photosynthetic bacteria
- The Proterozoic period (2.5 bya - 0.6 bya), where single-celled (~1.8 bya) then multicellular eukaryotes (~1 bya) form. After multicellular eukayrotes, animals emerge toward the end of the Proterozoic era (750 mya)
- The last period, the Phanerozoic period (~600 mya- present) is constructed into three subgroups: the Paleozoic, Mesozoic, and Cenozoic eras, where the colonization of land and humans emerged.
Stromatolites
Oldest known fossils; which are mats of cyanobacteria, new generations form on top of older. ~3.5 billion years old
Prokaryotes were sole inhabitants for more than 1.5 billion years
Endosymbiont theory
Where the first Eukaryotes are hypothesized to come from, where a prokaryote engulfs a small cell that evolved into a mitochondrion
Endosymbiont
The small cell that was engulfed and lived within the cell that engulfed it, which was the host cell