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Journal Cover Nature Geoscience
  Journal Prestige (SJR): 7.297
  Citation Impact (citeScore): 111
  Number of Followers: 287  
    
   Full-text available via subscription Subscription journal
   ISSN (Print) 1752-0894 - ISSN (Online) 1752-0908
   Published by NPG Homepage  [143 journals]
  • Improved efficiency of the biological pump as a trigger for the Late
           Ordovician glaciation
    • Improved efficiency of the biological pump as a trigger for the Late Ordovician glaciation

      Improved efficiency of the biological pump as a trigger for the Late Ordovician glaciation, Published online: 11 June 2018; doi:10.1038/s41561-018-0141-5

      Enhanced algal productivity during the Late Ordovician may have led to carbon drawdown and the inception of the Hirnantian glaciation, according to sediment geochemistry and carbon cycle modelling.Improved efficiency of the biological pump as a trigger for the Late Ordovician glaciation, Published online: 2018-06-11; doi:10.1038/s41561-018-0141-52018-06-11
      DOI: 10.1038/s41561-018-0141-5
       
  • Constraining ocean transport
    • Constraining ocean transport

      Constraining ocean transport, Published online: 11 June 2018; doi:10.1038/s41561-018-0165-x

      Accounting for the oceanic transport of carbon suggests that existing estimates of the location and magnitude of the land carbon sinks need to be revised.Constraining ocean transport, Published online: 2018-06-11; doi:10.1038/s41561-018-0165-x2018-06-11
      DOI: 10.1038/s41561-018-0165-x
       
  • Revision of global carbon fluxes based on a reassessment of oceanic and
           riverine carbon transport
    • Revision of global carbon fluxes based on a reassessment of oceanic and riverine carbon transport

      Revision of global carbon fluxes based on a reassessment of oceanic and riverine carbon transport, Published online: 11 June 2018; doi:10.1038/s41561-018-0151-3

      Terrestrial carbon sources in the Southern Hemisphere and sinks in the Northern Hemisphere may be smaller than thought, according to a recalculation that accounts for the oceanic redistribution of carbon.Revision of global carbon fluxes based on a reassessment of oceanic and riverine carbon transport, Published online: 2018-06-11; doi:10.1038/s41561-018-0151-32018-06-11
      DOI: 10.1038/s41561-018-0151-3
       
  • Drivers and mechanisms of ocean deoxygenation
    • Drivers and mechanisms of ocean deoxygenation

      Drivers and mechanisms of ocean deoxygenation, Published online: 11 June 2018; doi:10.1038/s41561-018-0152-2

      Ocean oxygen loss in a warming world is strongly affected by biogeochemical processes that are not fully accounted for in ocean models, suggests a literature synthesis.Drivers and mechanisms of ocean deoxygenation, Published online: 2018-06-11; doi:10.1038/s41561-018-0152-22018-06-11
      DOI: 10.1038/s41561-018-0152-2
       
  • Author Correction: The global volume and distribution of modern
           groundwater
    • Author Correction: The global volume and distribution of modern groundwater

      Author Correction: The global volume and distribution of modern groundwater, Published online: 11 June 2018; doi:10.1038/s41561-018-0164-y

      Author Correction: The global volume and distribution of modern groundwaterAuthor Correction: The global volume and distribution of modern groundwater, Published online: 2018-06-11; doi:10.1038/s41561-018-0164-y2018-06-11
      DOI: 10.1038/s41561-018-0164-y
       
  • Author Correction: Reduced air–sea CO2 exchange in the Atlantic Ocean
           due to biological surfactants
    • Author Correction: Reduced air–sea CO2 exchange in the Atlantic Ocean due to biological surfactants

      Author Correction: Reduced air–sea CO2 exchange in the Atlantic Ocean due to biological surfactants, Published online: 06 June 2018; doi:10.1038/s41561-018-0173-x

      Author Correction: Reduced air–sea CO2 exchange in the Atlantic Ocean due to biological surfactantsAuthor Correction: Reduced air–sea CO2 exchange in the Atlantic Ocean due to biological surfactants, Published online: 2018-06-06; doi:10.1038/s41561-018-0173-x2018-06-06
      DOI: 10.1038/s41561-018-0173-x
       
  • Publisher Correction: Modification of the Western Gondwana craton by
           plume–lithosphere interaction
    • Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction

      Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction, Published online: 05 June 2018; doi:10.1038/s41561-018-0163-z

      Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interactionPublisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction, Published online: 2018-06-05; doi:10.1038/s41561-018-0163-z2018-06-05
      DOI: 10.1038/s41561-018-0163-z
       
  • Thermal effects of pyroxenites on mantle melting below mid-ocean ridges
    • Thermal effects of pyroxenites on mantle melting below mid-ocean ridges

      Thermal effects of pyroxenites on mantle melting below mid-ocean ridges, Published online: 04 June 2018; doi:10.1038/s41561-018-0139-z

      Pyroxenite—recycled, subducted material—beneath mid-ocean ridges cools the mantle, suppressing melt extraction and crust formation, according to geochemical analyses of samples taken from the Mid-Atlantic Ridge.Thermal effects of pyroxenites on mantle melting below mid-ocean ridges, Published online: 2018-06-04; doi:10.1038/s41561-018-0139-z2018-06-04
      DOI: 10.1038/s41561-018-0139-z
       
 
 
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