ASTR/GEOL-2040: Search for life in the Universe: Lecture 15

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Presentation transcript:

ASTR/GEOL-2040: Search for life in the Universe: Lecture 15 Geological record Fossil record Early oceans & life ASTR-2040: Lecture 15, Oct 4, 2017 Axel Brandenburg (Office hours: Mondays 2:30 – 3:30 in X590 and Wednesdays 11-12 in D230)

Reading the geological record Written history 5.4 kyr (3400 BC) Geological record 4 Gyr

Perspective Football stadium 50 m  5 Gyr This room 5 m  500 Myr 5 cm  5 Myr 5 mm  500,000 yr But written record only 5000 yr.

If 5 Gyr = 50 m, then what is 5000 yr?

If 5 Gyr = 50 m, then what is 5000 yr? 6 orders of magnitude, so 5 kyr  50 mm

Rock types Igneous metamorphic sedimentary From molten rock  cools, solidifies metamorphic Not from molten, but altered (chem & struct) by pressure & temperature sedimentary Compression of sediments

Igneous rocks Felsic Mafic granite gabbro basalt > 63% SiO2 ~2.7 g/cm3 Mafic < 52% SiO2 ~3.0 g/cm3

Sedimentary rock Igneous

More sedimentary rocks Here: limestone CaCO3

Metamorphic rocks Here: limestone CaCO3

The Giant Impact Theory The Moon forming event ~4.5 Ga

Billions and billions of years ago... Numerous Mars-sized objects orbiting the Sun. Occasional impacts with protoplanets are believed to have produced some interesting results: Mercury’s large iron core Venus’ awkward rotation Earth’s moon

The set-up Proto-Earth is orbiting the young Sun at approximately its current distance. A Mars-sized planetoid, often termed Theia, strikes proto-Earth at a glancing blow. Both bodies are liquified: Most of Theia’s rocky mantle and a bit of its iron core are ejected into orbit. The remaining material accretes back onto Earth. Roughly one year later, the Moon has mostly accreted from the material in orbit around the Earth.

Geological record

Now we play the waiting game... After formation, the Moon stays in Earth’s orbit. The Moon experienced the full force of the Late Heavy Bombardment (LHB), responsible for the formation of the lunar maria. Lunar volcanism completely ceased as late as 1 Gyr ago. The Moon’s surface has been, and continues to be, a target for asteroids and meteors crossing its path since its formation.

Another Movie! Life of the Moon - NASA GSFC

Geological record

What type of rock on the Moon? Granite Basalt Marble Sandstone Limestone

Comparison with fossils Fossils from mineral-rich portions Or filled w/ mineral-rich water Minerals cast shape Apex Chert in Pilbara, Craton

Fossils Apex Chert in Pilbara, Craton

Cherts Microcrystalline sedimentary rock Silica-rich Resist metamorphism Example next: Apex Chert Apex Chert in Pilbara, Craton

Fossil evidence for life Apex Chert in Pilbara, Craton

Fossil evidence for life Apex Chert in Pilbara, Craton Nature 260, 640 (1993)

Fossil evidence for life Apex Chert in Pilbara, Craton

Isotope fingerprints on fossils Carbonate carbon Always ~0 Organic carbon -20 … -30 per mil Apex Chert in Pilbara, Craton

Look at age No trend with age Apex Chert in Pilbara, Craton

Next time Hydrothermal vents Cambrian explosion of life RGS box 2.6, plate 2.19 Longstaff 223 – 233

Next time Hydrothermal vents Cambrian explosion of life RGS box 2.6, plate 2.19 Longstaff 223 – 233