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Showing 1–15 of 15 results
Advanced filters: Author: Tim DeVries Clear advanced filters

  • Biological uptake in the surface and release in the deep ocean contribute to oceanic nickel distribution, including the residual surface Ni pool, according to culture experiments, field data and global biogeochemical circulation modelling

    • Seth G. John
    • Rachel L. Kelly
    • Shun-Chung Yang
    Research
    Nature Geoscience
    Volume: 15, P: 906-912

  • Stress on land is dynamic, entailing swift and drastic changes. Integrated time-course stress and co-expression analysis predict a gene regulatory network that retraces a web of ancient signal convergences shared by land plants and their algal sisters.

    • Tim P. Rieseberg
    • Armin Dadras
    • Jan de Vries
    ResearchOpen Access
    Nature Communications
    Volume: 16, P: 1-19

  • In a large, partially prospective cohort of patients with molecularly profiled and clinically annotated meningioma, the extent of surgical resection and radiotherapy (RT) response correlate with molecular classification, which can be used in a molecular model to predict clinical outcomes in response to RT.

    • Justin Z. Wang
    • Vikas Patil
    • Gelareh Zadeh
    ResearchOpen Access
    Nature Medicine
    Volume: 30, P: 3173-3183

  • The elemental composition of marine organic matter varies systematically at large scales. Simulations of the ocean circulation and observations of ocean chemistry reveal close links between light and nutrient availability and stoichiometry.

    • Tim DeVries
    • Curtis Deutsch
    Research
    Nature Geoscience
    Volume: 7, P: 890-894

  • Soils from 30 grasslands across Europe were subjected to 4 contrasting extreme climatic events under drought, flood, freezing and heat conditions, with the results suggesting that soil microbiomes from different climates share unified responses to extreme climatic events.

    • Christopher G. Knight
    • Océane Nicolitch
    • Franciska T. de Vries
    ResearchOpen Access
    Nature
    Volume: 636, P: 690-696

  • Dadras et al. exposed Mesotaenium, an alga of the sister lineage to land plants, to a bifactorial gradient of environmental cues and use comparative analyses to pinpoint conserved circuits in plant genetic response networks.

    • Armin Dadras
    • Janine M. R. Fürst-Jansen
    • Jan de Vries
    ResearchOpen Access
    Nature Plants
    Volume: 9, P: 1419-1438

  • Upwelling of CO2 from the Southern Ocean may have played a key role in deglacial warming, but marine sediment studies are hindered by inaccurate chronologies. Siani et al. present new surface reservoir 14C ages derived from tephra and show that deglacial CO2escape was synchronous with Antarctic warming.

    • Giuseppe Siani
    • Elisabeth Michel
    • Anna Lourantou
    Research
    Nature Communications
    Volume: 4, P: 1-9

  • The deep North Pacific is the end of the road for global ocean circulation, but the circulation patterns and ventilation are poorly understood. Here the authors show that diffusive transports both along and across density layers play a leading role in returning 1,400 year old water to the surface.

    • Mark Holzer
    • Tim DeVries
    • Casimir de Lavergne
    ResearchOpen Access
    Nature Communications
    Volume: 12, P: 1-13

  • Carbon uptake by the ocean has increased alongside rising atmospheric CO2 concentrations, but with substantial variability. This Review examines trends in ocean CO2 uptake and the internal and external factors driving its variability, finding an ocean uptake of –2.7 ± 0.3 Pg C year–1 for the period 1990 through 2019.

    • Nicolas Gruber
    • Dorothee C. E. Bakker
    • Jens Daniel Müller
    Reviews
    Nature Reviews Earth & Environment
    Volume: 4, P: 119-134

  • The elemental ratios of marine phytoplankton and organic matter vary widely across ocean biomes, according to a catalogue of biogeochemical data, suggesting that climate change may have complex effects on the ocean’s elemental cycles.

    • Tim DeVries
    News & Views
    Nature Geoscience
    Volume: 11, P: 15-16

  • Modelling of ocean carbon uptake for the 1980s to the 2000s shows that stronger upper-ocean overturning caused less carbon to be absorbed by the oceans in the 1990s, but that as the overturning circulation weakens more carbon is now being absorbed.

    • Tim DeVries
    • Mark Holzer
    • Francois Primeau
    Research
    Nature
    Volume: 542, P: 215-218