The naked planet Earth:
Most essential pre-requisite for the origin and evolution of life
Our blue
planet Earth has long been regarded to carry full of nutrients for
hosting life since the birth of the planet. Here we speculate the
processes that led to the birth of early life on Earth and its
aftermath, finally leading to the evolution of metazoans. We evaluate:
(1) the source of nutrients, (2) the chemistry of primordial ocean, (3)
the initial mass of ocean, and (4) the size of planet. Among the
life-building nutrients, phosphorus and potassium play a key role. Only
three types of rocks can serve as an adequate source of nutrients: (a)
continent-forming TTG (granite), enabling the evolution of primitive
life to metazoans; (b) primordial continents carrying anorthosite with
KREEP (Potassium, Rare Earth Elements, and Phosphorus) basalts, which is
a key to bear life; (c) carbonatite magma, enriched in radiogenic
elements such as U and Th, which can cause mutation to speed up
evolution and promote the birth of new species in continental rift
settings. The second important factor is ocean chemistry. The primordial
ocean was extremely acidic (pH = 1–2) and enriched in halogens (Cl, F
and others), S, N and metallic elements (Cd, Cu, Zn, and others),
inhibiting the birth of life. Plate tectonics cleaned up these elements
which interfered with RNA. Blue ocean finally appeared in the
Phanerozoic with pH = 7 through extensive interaction with surface
continental crust by weathering, erosion and transportation into ocean.
The initial ocean mass was also important. The birth of life and
aftermath of evolution was possible in the habitable zone with 3–5 km
deep ocean which was able to supply sufficient nutrients. Without a huge
landmass, nutrients cannot be supplied into the ocean only by
ridge-hydrothermal circulation in the Hadean. Finally, the size of the
planet plays a crucial role. Cooling of massive planets is less
efficient than smaller ones, so that return-flow of seawater into mantle
does not occur until central stars finish their main sequence. Due to
the suitable size of Earth, the dawn of Phanerozoic witnessed the
initiation of return-flow of seawater into the mantle, leading to the
emergence of huge landmass above sea-level, and the distribution of
nutrients on a global scale. Oxygen pump also played a critical role to
keep high-PO2 in atmosphere since then, leading to the emergence of ozone layer and enabling animals and plants to invade the land.
http://www.sciencedirect.com/science/article/pii/S1674987112001272
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