Substantial role of macroalgae in marine carbon sequestration
By D. Krause‐Jensen, Carlos M. Duarte. 2016
967 citations recorded by the source corpus.
Subfields: Ecology, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/2e81fe3d40e89772eaabb83ee8741df7f94f6f4e
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- A. Queirós
- D. Krause‐Jensen
- A. Atkinson
- I. Chung
- P. Somerfield
- Steve Widdicombe
- John Beardall
- R. Airs
In Global and Planetary Change
- A. Queirós
- A. Atkinson
- C. Pascoe
- A. Beesley
- P. Somerfield
- P. Lindeque
- Steve Widdicombe
- John Beardall
In Oceanography
- A. Queirós
- D. Krause‐Jensen
- A. Atkinson
- C. Pascoe
- A. Beesley
- I. Chung
- P. Somerfield
- Steve Widdicombe
Citations in the corpus
- Connected macroalgal‐sediment systems: blue carbon and food webs in the deep coastal ocean (2019, background): “Further measurements of dissolved organic carbon production generated by macroalgal communities, and its potential benthic uptake (which we did not measure) could further increase global significance of the sequestration fluxes we estimate (Krause-Jensen and Duarte 2016).”
- Substantial seagrass blue carbon pools in the southwestern Baltic Sea are spatially heterogeneous, mostly autochthonous, and include relics of terrestrial peatlands (2022, background): “…coastal vegetated ecosystems, like seagrass meadows, mangrove forests, and tidal salt marshes, account for almost half of the total organic carbon (Corg) buried in marine sediments (Duarte et al. 2005, Mcleod et al. 2011, Krause-Jensen and Duarte 2016), collectively estimated to mitigate approx.”
- The future of seaweed aquaculture in a rapidly changing world (2017, background): “The estimate of Krause-Jensen & Duarte (2016) of about 173 Tg C year–1 (with a range of 61–268 Tg C year–1) fixed by seaweeds globally is a relatively small proportion of total oceanic primary production (54–59 Pg C year–1) and the increase in atmospheric CO2 of 4 Pg C year −1 (Denman et al., 2007).”