Results 121 to 130 of about 2,704 (186)

Chance and purpose in the evolution of biospheres. [PDF]

open access: yesPhilos Trans R Soc Lond B Biol Sci
Donoghue PCJ   +4 more
europepmc   +1 more source

Marine sulphate captures a Paleozoic transition to a modern terrestrial weathering environment. [PDF]

open access: yesNat Commun
Waldeck AR   +11 more
europepmc   +1 more source

Channelized metasomatism in Archean cratonic roots as a mechanism of lithospheric refertilization. [PDF]

open access: yesNat Commun
Roots EA   +6 more
europepmc   +1 more source

Evolution of the iodine cycle and the late stabilization of the Earth's ozone layer. [PDF]

open access: yesProc Natl Acad Sci U S A
Liu J   +4 more
europepmc   +1 more source

End of the Proterozoic Eon

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.
openaire   +2 more sources

The Golden Proterozoic

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

Home - About - Disclaimer - Privacy