News & Views |
Featured
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Article |
Assimilation of upwelled nitrate by small eukaryotes in the Sargasso Sea
Low levels of biologically available forms of nitrogen can limit phytoplankton growth. Isotopic analyses of seawater samples collected from the Sargasso Sea in the summer suggest that small phytoplankton obtain half of their nitrogen from upwelled nitrate.
- Sarah E. Fawcett
- , Michael W. Lomas
- & Daniel M. Sigman
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Letter |
Dust- and mineral-iron utilization by the marine dinitrogen-fixer Trichodesmium
Blooms of the nitrogen-fixing cyanobacterium Trichodesmium, which fuel primary production in tropical and subtropical waters, require large quantities of iron. Laboratory incubations suggest that Trichodesmium accelerates the dissolution of iron oxides and dust, increasing the rate of iron uptake.
- Maxim Rubin
- , Ilana Berman-Frank
- & Yeala Shaked
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News & Views |
Breathing room for early animals
Animals originated in a world with marine oxygen levels only a fraction of those found in today's oceans. Observations of microbial habitats in present-day lagoons suggest that early animals could have found refuge in oxygen-producing mats.
- Jake Bailey
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News & Views |
Marine mercury breakdown
The neurotoxin methylmercury accumulates in marine biota and their predators. An analysis of seabird egg shells suggests that sea-ice cover reduces the breakdown of this highly toxic compound in sea water.
- Joel D. Blum
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News & Views |
Ocean algae and atmospheric ice
Mineral dust and biological particles of terrestrial origin initiate ice formation in the atmosphere. Laboratory experiments suggest that ocean diatoms are another potential source of ice nuclei in clouds.
- Ottmar Möhler
- & Corinna Hoose
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Article |
Methylmercury photodegradation influenced by sea-ice cover in Arctic marine ecosystems
Atmospheric deposition of mercury to remote areas has increased threefold since pre-industrial times. Reductions in sea-ice cover accelerate the photodegradation of biologically accessible mercury in Arctic waters, according to an analysis of the isotopic composition of bird eggs in northern latitudes.
- D. Point
- , J. E. Sonke
- & P. R. Becker
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News & Views |
Carbon cycle at depth
The existence of a microbial community in the ocean crust has long been hypothesized. Isotopic evidence indicates that a deep biosphere of microbes both scrubs oceanic fluids of organic matter and produces new, yet old, organic carbon in situ.
- Katrina J. Edwards
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Letter |
Stimulation of ice nucleation by marine diatoms
Biogenic aerosol particles of terrestrial origin, including bacteria and pollen, trigger ice formation in the atmosphere. Laboratory experiments reveal that biogenic particles of marine origin also initiate ice formation under typical tropospheric conditions.
- D. A. Knopf
- , P. A. Alpert
- & J. Y. Aller
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Letter |
Sedimentary membrane lipids recycled by deep-sea benthic archaea
Archaea are prevalent in the deep sea, and comprise a major fraction of the biomass in marine sediments. 13C-labelling experiments on the sea floor suggest that benthic archaea use sedimentary organic compounds to construct their membranes.
- Yoshinori Takano
- , Yoshito Chikaraishi
- & Naohiko Ohkouchi
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Commentary |
A count in the dark
The Census of Marine Life has succeeded in raising awareness about marine biodiversity, and contributed much to our understanding of what lives where. But the project has fallen short of its goal to estimate species abundance.
- Daniel Pauly
- & Rainer Froese
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Editorial |
Phytoplankton flounder
The foundation of the marine food web is faltering, according to a century-long data set.
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News & Views |
Safer in the south
Many species of nannoplankton with carbonate shells vanished during the mass extinction 65 million years ago. An analysis of extinction rates from the world's oceans reveals a geographic bias in the demise and recovery of nannoplankton species.
- Paul B. Wignall
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News & Views |
Patterns of tropical warming
The effect of rising greenhouse-gas emissions on climate is not uniform across the globe. An analysis of the mechanisms behind model-projected changes in ocean temperature gives greater confidence in the pattern of tropical warming and its potential impacts.
- Amy C. Clement
- , Andrew C. Baker
- & Julie Leloup