Results 1 to 10 of about 15,483 (211)

Comments on “was hydrogen peroxide present before the arrival of oxygenic photosynthesis? The important role of iron(II) in the archean ocean”

open access: yesRedox Biology
Recent research has hypothesized that hydrogen peroxide (H2O2) may have emerged from abiotic geochemical processes during the Archean eon (4.0–2.5 Ga), stimulating the evolution of an enzymatic antioxidant system in early life. This eventually led to the
Xiao Wu   +4 more
doaj   +1 more source

The Detectability of CH4/CO2/CO and N2O Biosignatures Through Reflection Spectroscopy of Terrestrial Exoplanets

open access: yesThe Astronomical Journal
The chemical makeup of Earth’s atmosphere during the Archean (4–2.5 Ga) and Proterozoic eon (2.5–0.5 Ga) contrast considerably with the present-day: the Archean was rich in carbon dioxide and methane, and the Proterozoic had potentially higher amounts of
Armen Tokadjian, Renyu Hu, Mario Damiano
doaj   +1 more source

Secular Changes in the Occurrence of Subduction During the Archean

open access: yesGeophysical Research Letters
Subduction processes play a pivotal role in facilitating material exchange between the crust and mantle, contributing to the growth of continents. However, the onset and evolution of subduction remain hotly debated.
Chun‐Tao Liu   +2 more
doaj   +1 more source

Quantitative study on vertical distribution of heat flow in Niutuozhen geothermal field, Xiong'an New Area—Evidence from heat flow determination in the Archean of D01 well

open access: yesJournal of Groundwater Science and Engineering
The karst geothermal reservoir in Xiong'an New Area is a representative example of an ancient buried hill geothermal system. However, published heat flow data are predominantly derived from the Cenozoic sedimentary cap.
Ya-hui Yao   +7 more
doaj   +1 more source

Data‐Driven Investigation Reveals Subaerial Proportion of Basalts Since the Early Archean

open access: yesGeophysical Research Letters
The subaerial exposure of the modern continental crust through time remains intensely debated, with estimates of the first exposure ranging from the late Archean to the Neoproterozoic.
Chun‐Tao Liu   +2 more
doaj   +1 more source

Giant lithium-rich pegmatites in Archean cratons form by remelting refertilised roots of greenstone belts

open access: yesCommunications Earth & Environment
Around 80% of the world’s hard-rock lithium supply comes from pegmatites formed in the Archean Eon, yet our understanding of how Lithium-pegmatites form assumes magma source compositions not relevant to those Archean cratons hosting most of the giant ...
Robert H. Smithies   +11 more
doaj   +1 more source

Links between the Archean hydrosphere and Earth's interior. [PDF]

open access: yesNat Commun
Long ZY   +6 more
europepmc   +1 more source

Coupled sulfur-silicon isotopes reveal supracrustal origin of Archean continents. [PDF]

open access: yesNat Commun
Shang K   +8 more
europepmc   +1 more source

Modern arc-like water content in the source of 3.1-billion-year-old volcanic rocks. [PDF]

open access: yesNat Commun
Vandenburg ED   +6 more
europepmc   +1 more source

Author Correction: Coupled sulfur-silicon isotopes reveal supracrustal origin of Archean continents. [PDF]

open access: yesNat Commun
Shang K   +8 more
europepmc   +1 more source

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