Recalcitrant dissolved organic carbon fractions.

By Dennis A. Hansell. Annual Review of Marine Science, 2013

789 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/68f6c75a67ab009fb8842a3cd670298fe90a35b2

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. C. Robinson
2. C. R. Lovell
3. Jorn Bruggeman
4. G. Kattner
5. J. D. Kinsey
6. Astrid Schnetzer
7. Michael J. Follows
8. C. Osburn

In Oceanography

1. C. Robinson
2. U. Passow
3. Farooq Azam
4. Hongyue Dang
5. C. R. Lovell
6. B. Koch
7. L. Legendre
8. G. Kattner

Citations in the corpus

• A physically based framework for modeling the organic fractionation of sea spray aerosol from bubble film Langmuir equilibria (2014, methodology): “We have chosen five broad classes of macromolecules: a lipid-like mixture associated with labile DOC, a polysaccharide-like mixture associated primarily with semilabile DOC, a proteinlike mixture with concentrations intermediate between lipids and polysaccharides, a processed mixture associated with”
• Molecular insights into the microbial formation of marine dissolved organic matter: recalcitrant or labile? (2014, background): “Refractory dissolved organic matter (DOM) in the oceans represents a large reservoir of organic carbon in the global carbon cycle (642 Pg C, Hansell, 2013).”
• Microbial Surface Colonization and Biofilm Development in Marine Environments (2015, background): “DOC (up to 662 Pg C) forms the largest organic carbon pool in the modern ocean, and a substantial fraction ( 97%) of DOC consists of refractory and ultrarefractory molecules that persist for thousands of years in the marine environment (286).”
• Formation of Chromophoric Dissolved Organic Matter by Bacterial Degradation of Phytoplankton-Derived Aggregates (2018, background): “Finally, hydrolytic enzymatic rates suggest that the bacterial community actively transforms organic matter with significant turnover of carbon and nitrogen, making bacteriallymediated production of RDOM from planktonic biomass a key pathway in global element cycles (e.g., Jiao et al., 2010; Lechten”
• ERSEM 15.06: a generic model for marine biogeochemistry and the ecosystem dynamics of the lower trophic levels (2015, background): “The formulation includes the bacteria-mediated production of recalcitrant DOC (Hansell, 2013) and therefore provides the conceptual framework for an implementation of the microbial carbon pump (Jiao et al.”
• Competition between photochemical and biological degradation of dissolved organic matter from the cyanobacteria Microcystis aeruginosa (2015, background): “The bioavailability of DOM can be described as a continuum, with pools that have half-lives from minutes to multiple millennia (Hansell 2013).”
• Rethinking the marine carbon cycle: Factoring in the multifarious lifestyles of microbes (2015, background): “Themarine DOM carbon pool is nearly equal to atmospheric CO2 and about 200 times that in living marine biomass (71).”
• Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “Accepting that limitation , assuming that the DOC concentration in the bathypelagic zone does not change substantially with depth (Hansell, 2013), the model can address the suggestion that RDOC is not directly transported to local bathypelagic zones, but moves with the thermohaline circulation and…”