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期刊名:Global biogeochemical cycles

缩写:GLOBAL BIOGEOCHEM CY

ISSN:0886-6236

e-ISSN:1944-9224

IF/分区:6.9/Q1

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共收录本刊相关文章索引68
Clinical Trial Case Reports Meta-Analysis RCT Review Systematic Review
Classical Article Case Reports Clinical Study Clinical Trial Clinical Trial Protocol Comment Comparative Study Editorial Guideline Letter Meta-Analysis Multicenter Study Observational Study Randomized Controlled Trial Review Systematic Review
Hong Chin Ng,Jon R Hawkings,Sebastien Bertrand et al. Hong Chin Ng et al.
Glacier meltwater supplies silicon (Si) and iron (Fe) sourced from weathered bedrock to downstream ecosystems. However, the extent to which these nutrients reach the ocean is regulated by the nature of the benthic cycling of dissolved Si an...
C Smeaton,W E N Austin C Smeaton
The sediments within fjords are critical components of the mid- to high-latitude coastal carbon (C) cycle, trapping and storing more organic carbon (OC) per unit area than other marine sedimentary environments. Located at the land-ocean tra...
Johan A Eckdahl,Pere Casal Rodriguez,Jeppe A Kristensen et al. Johan A Eckdahl et al.
Approximately 40% of earth's carbon (C) stored in land vegetation and soil is within the boreal region. This large C pool is subjected to substantial removals and transformations during periodic wildfire. Fire-altered C, commonly known as p...
Haidi Chen,F Alexander Haumann,Lynne D Talley et al. Haidi Chen et al.
The deep ocean releases large amounts of old, pre-industrial carbon dioxide (CO2) to the atmosphere through upwelling in the Southern Ocean, which counters the marine carbon uptake occurring elsewhere. This Southern Ocean CO2 release is rel...
Francisco de Melo Viríssimo,Adrian P Martin,Stephanie A Henson Francisco de Melo Viríssimo
The biological carbon pump is a key component of the marine carbon cycle. This surface-to-deep flux of carbon is usually assumed to follow a simple power law function, which imposes that the surface export flux is attenuated throughout subs...
Ying-Ping Wang,Yuanyuan Huang,Laurent Augusto et al. Ying-Ping Wang et al.
The representation of phosphorus (P) cycling in global land models remains quite simplistic, particularly on soil inorganic phosphorus. For example, sorption and desorption remain unresolved and their dependence on soil physical and chemica...
Dustin Carroll,Dimitris Menemenlis,Stephanie Dutkiewicz et al. Dustin Carroll et al.
The inventory and variability of oceanic dissolved inorganic carbon (DIC) is driven by the interplay of physical, chemical, and biological processes. Quantifying the spatiotemporal variability of these drivers is crucial for a mechanistic u...
Yeala Shaked,Benjamin S Twining,Alessandro Tagliabue et al. Yeala Shaked et al.
We present a new approach for quantifying the bioavailability of dissolved iron (dFe) to oceanic phytoplankton. Bioavailability is defined using an uptake rate constant (kin-app) computed by combining data on: (a) Fe content of individual i...
Nicholas Bock,Marin Cornec,Hervé Claustre et al. Nicholas Bock et al.
Biogeographical classifications of the global ocean generalize spatiotemporal trends in species or biomass distributions across discrete ocean biomes or provinces. These classifications are generally based on a combination of remote-sensed ...
Colleen A Durkin,Ken O Buesseler,Ivona Cetinić et al. Colleen A Durkin et al.
To better quantify the ocean's biological carbon pump, we resolved the diversity of sinking particles that transport carbon into the ocean's interior, their contribution to carbon export, and their attenuation with depth. Sinking particles ...