Early Chemical Evidence of Life Flashcards

(16 cards)

1
Q

If life evolved prior to first microfossil evidence, how can we identify it?

A

geochemical signatures in the organic fraction of rocks

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2
Q

kerogen

A

heterogenous, high molecular weight organic mixture formed when organic carbon of dead organisms undergoes diagenesis

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3
Q

what is a key to the search for chemical evidence of life

A

kerogen

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4
Q

isotope

A

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

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5
Q

kinetic isotope effect

A

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

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6
Q

what scale is difference in kinetic energy between isotopes stated

A

ratio to a standard in per mil delta notation
(example delta ^13C = -40 0/00 or delta ^13C = 10 0/00)

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7
Q

reference for standard for Carbon 13

A

belemnite from PeeDee Formation

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8
Q

How can delta ^13C = -40 0/00 be expressed in words

A

enriched in carbon 12 or depleted in carbon 13 (because of negative value of the ratio of C13/C12)

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9
Q

How do isotopes provide evidence for life?

A

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

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10
Q

Where in the autotroph processes does carbon isotope fractionation take place?

A

1 - diffusion of inorganic carbon into the cell
2 - fixing the inorganic carbon into organic carbon

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11
Q

signature in rock that helps to identify biogenic processes

A

Kerogen that in enriched in light carbon isotopes as compared to the associated reservoir of inorganic carbon that is enriched in heavy carbon isotopes

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12
Q

rough fractionation that can be produced by autotrophic microbes

A

20 0/00

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13
Q

Hadean chemical signatures

A

4.4 Ga Jack Hills Zircon
Light carbon in graphite inclusion
not claiming life, just organic
contested

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14
Q

earliest Archean chemical signature

A

3.85 Akilia Greenland
light carbon in graphite inclusions in apatite
back and forth, most recent conclusion is sedimentary BIF with light graphite

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15
Q

partial Archean chemical signature

A

3.8 Isua, Greenland
metamorphosed shale
graphite enriched in C12 but no reservoir to compare to

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16
Q

Archean chemical evidence of life

A

3.5 Coonterunah, Australia
Kerogenous limestone
light carbon Kerogen with carbonate reservoir showing a fractionation of 20 0/00
convincing evidence of autotrophic activity