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Chance and purpose in the evolution of biospheres. [PDF]
Donoghue PCJ +4 more
europepmc +1 more source
Enhanced metamorphic CO<sub>2</sub> release on the Proterozoic Earth. [PDF]
Stewart EM, Penman DE.
europepmc +1 more source
Three-dimensional reconstruction of ediacaran ceramiales (Rhodophyta) from the phosphorite doushantuo formation, South China. [PDF]
Du W +5 more
europepmc +1 more source
Marine sulphate captures a Paleozoic transition to a modern terrestrial weathering environment. [PDF]
Waldeck AR +11 more
europepmc +1 more source
Impact of steroid biosynthesis on the aerobic adaptation of eukaryotes. [PDF]
Hoshino Y, Gaucher EA.
europepmc +1 more source
Channelized metasomatism in Archean cratonic roots as a mechanism of lithospheric refertilization. [PDF]
Roots EA +6 more
europepmc +1 more source
Evolution of the iodine cycle and the late stabilization of the Earth's ozone layer. [PDF]
Liu J +4 more
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Scientific American, 1991
Living organisms have inhabited the surface of our planet for nearly four billion years. Yet the plants and animals that define our everyday existence have far more recent origins. The ancestors of modern trees and terrestrial animals first colonized land only about 450 million years ago.
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Living organisms have inhabited the surface of our planet for nearly four billion years. Yet the plants and animals that define our everyday existence have far more recent origins. The ancestors of modern trees and terrestrial animals first colonized land only about 450 million years ago.
openaire +2 more sources
1982
The Dominion Group, Witwatersrand Supergroup, and Ventersdorp Supergroup constitute a volcanosedimentary sequence that is famous for its fossil gold placers. It has been estimated that since gold-bearing conglomerates were discovered near Johannesburg (Fig. 4-1) in 1886, mines in the Transvaal and Orange Free State have produced more than 55 percent of
A. J. Tankard +5 more
openaire +1 more source
The Dominion Group, Witwatersrand Supergroup, and Ventersdorp Supergroup constitute a volcanosedimentary sequence that is famous for its fossil gold placers. It has been estimated that since gold-bearing conglomerates were discovered near Johannesburg (Fig. 4-1) in 1886, mines in the Transvaal and Orange Free State have produced more than 55 percent of
A. J. Tankard +5 more
openaire +1 more source

