High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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Early photosynthetic eukaryotes inhabited low-salinity habitats.

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P2860

High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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P1476

High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment

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P2093

John Parnell

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Stephen Bowden

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Steven Andrews

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Wanethon Thayalan

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P2860

History of biological metal utilization inferred through phylogenomic analysis of protein structures

Proterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge?

Morphological and ecological complexity in early eukaryotic ecosystems.

General trends in trace element utilization revealed by comparative genomic analyses of Co, Cu, Mo, Ni, and Se.

Earth's earliest non-marine eukaryotes.

Molybdenum cofactors, enzymes and pathways.

Proterozoic ocean redox and biogeochemical stasis.

Ocean oxygenation in the wake of the Marinoan glaciation.

Tracing the stepwise oxygenation of the Proterozoic ocean.

Potential Trace Metal Co-Limitation Controls on N2 Fixation and [Formula: see text] Uptake in Lakes with Varying Trophic Status.

P2888

ncomms7996

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6996

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scholarly article

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10.1038/NCOMMS7996

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English

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Samuel Spinks

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2015-05-19T00:00:00Z

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276921766

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25988499

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2015NatCo...6.6996P

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High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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P2860

P2860

High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment.

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P1476

P2093

P2860

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