Early Chemical Evidence of Life Flashcards
(16 cards)
If life evolved prior to first microfossil evidence, how can we identify it?
geochemical signatures in the organic fraction of rocks
kerogen
heterogenous, high molecular weight organic mixture formed when organic carbon of dead organisms undergoes diagenesis
what is a key to the search for chemical evidence of life
kerogen
isotope
different form of the same element (same number of protons and electrons) with different number of neutrons - changes the molecular weight of the element-
same electronic structure and behave in nearly the same manner
kinetic isotope effect
heavier isotopes (more neutrons) will react more slowly than lighter isotopes, impacting the kinetic behavior of the isotopes, leading to a natural separation in isotopes
what scale is difference in kinetic energy between isotopes stated
ratio to a standard in per mil delta notation
(example delta ^13C = -40 0/00 or delta ^13C = 10 0/00)
reference for standard for Carbon 13
belemnite from PeeDee Formation
How can delta ^13C = -40 0/00 be expressed in words
enriched in carbon 12 or depleted in carbon 13 (because of negative value of the ratio of C13/C12)
How do isotopes provide evidence for life?
Life is lazy - autotrophs will use the light carbon first because it takes less energy to use it, leaving a reservoir enriched in the heavier C13 isotope
Where in the autotroph processes does carbon isotope fractionation take place?
1 - diffusion of inorganic carbon into the cell
2 - fixing the inorganic carbon into organic carbon
signature in rock that helps to identify biogenic processes
Kerogen that in enriched in light carbon isotopes as compared to the associated reservoir of inorganic carbon that is enriched in heavy carbon isotopes
rough fractionation that can be produced by autotrophic microbes
20 0/00
Hadean chemical signatures
4.4 Ga Jack Hills Zircon
Light carbon in graphite inclusion
not claiming life, just organic
contested
earliest Archean chemical signature
3.85 Akilia Greenland
light carbon in graphite inclusions in apatite
back and forth, most recent conclusion is sedimentary BIF with light graphite
partial Archean chemical signature
3.8 Isua, Greenland
metamorphosed shale
graphite enriched in C12 but no reservoir to compare to
Archean chemical evidence of life
3.5 Coonterunah, Australia
Kerogenous limestone
light carbon Kerogen with carbonate reservoir showing a fractionation of 20 0/00
convincing evidence of autotrophic activity