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  • 1
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    Physiological responses of a Southern Ocean diatom to complex future ocean conditions (2016)
    Springer Nature
    Details
    Publication Date: 2016-01-28
    Description: Investigation of multiple stressors on a subantarctic diatom reveals the importance of considering individual and interactive effects. Experiments show that temperature and iron enrichment enhance growth and help overcome nutrient depletion. Nature Climate Change 6 207 doi: 10.1038/nclimate2811
    Print ISSN: 1758-678X
    Electronic ISSN: 1758-6798
    Topics: Geosciences
    Published by Springer Nature
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  • 2
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    Metabolically-induced pH fluctuations by some coastal calcifiers exceed projected 22nd century ocean acidification: a mechanism for differential susceptibility? (2011)
    Wiley
    Details
    Publication Date: 2011-06-10
    Description: Anthropogenically-mediated decreases in pH, termed ocean acidification (OA), may be a major threat to marine organisms and communities. Research has focussed mainly on tropical coral reefs, but temperate reefs play a no less important ecological role in colder waters, where OA effects may first be manifest. Here, we report that trends in pH at the surface of three ecologically-important cold-water calcifiers (a primary producer and herbivores), under a range of fluid flows, differ substantially from one another, and for two of the three calcifiers the pH, during darkness, is lower than the mean projected pH due to OA for the surface waters of the global ocean beyond the year 2100. Using micro-optodes, we show that each calcifier had a different pH gradient between its surface and mainstream seawater, i.e. within the diffusion boundary layer which appears to act as an environmental buffer to mainstream pH. Abalone encountered only mainstream seawater pH, whereas pH at the sea urchins’ surface was reduced by ~0.35 units. For coralline algae, pH was ~0.5 units higher in the light and ~0.35 units lower under darkness than in ambient mainstream seawater. This wide range of pH within the DBL of some calcifiers will probably affect their performance under projected future reductions in pH due to OA. Differing exposure to a range of surface pH may result in differential susceptibility of calcifiers to OA. Such fluctuations are no doubt regulated by the interplay of water movement, morphology and metabolic rates (e.g. respiration, calcification and/or photosynthesis). Our study, by considering physics (flow regime), chemistry (pH gradients versus OA future projections) and biology (trophic level, physiology and morphology), reveals that predicting species-specific responses and subsequent ecosystem restructuring to OA is complex and requires a holistic, ecomechanical, approach.
    Print ISSN: 1354-1013
    Electronic ISSN: 1365-2486
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Published by Wiley
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  • 3
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    A ventilation-based framework to explain the regeneration – scavenging balance of iron in the Ocean (2014)
    Wiley
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    Publication Date: 2014-09-23
    Description: Our understanding of the processes driving the patterns of dissolved iron (DFe) in the ocean interior, either in observations or models, is complicated by the combined influences of subduction from the surface mixed-layer, notable subsurface sources, regeneration and scavenging loss. We describe a ventilation-based framework to quantify these processes in a global ocean biogeochemical model including diagnostics along potential density surfaces. There is a prevailing control of subsurface DFe by the subduction of surface DFe as preformed DFe augmented by benthic sources of DFe from hydrothermal activity and sediments. Unlike phosphate, there is a first order balance with a near cancellation between regeneration and scavenging with the remaining ‘net regeneration’ controlled by the ventilation of surface excesses in Fe-binding ligands. This DFe framework provides a more stringent test of how the total DFe distribution is mechanistically controlled within a model and may be subsequently used to interpret observed DFe distributions.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 4
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    Sinking velocities and microbial respiration rates alter the attenuation of particulate carbon fluxes through the mesopelagic zone (2015)
    Wiley
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    Publication Date: 2015-01-09
    Description: The attenuation of sinking particle fluxes through the mesopelagic zone is an important process that controls the sequestration of carbon and the distribution of other elements throughout the oceans. Case studies at two contrasting sites, the oligotrophic regime of the Bermuda Atlantic Time Series (BATS) and the mesotrophic waters of the western Antarctic Peninsula (WAP) sector of the Southern Ocean, revealed large differences in the rates of particle-attached microbial respiration and the average sinking velocities of marine particles, two parameters that affect the transfer efficiency of particulate matter from the base of the euphotic zone into the deep ocean. Rapid average sinking velocities of 270 ± 150 m d −1 were observed along the WAP, whereas the average velocity was 49 ± 25 m d −1 at the BATS site. Respiration rates of particle-attached microbes were measured using novel RESPIRE (REspiration of Sinking Particles In the subsuRface ocEan, Boyd et al., unpublished manuscript) sediment traps that first intercepts sinking particles then incubates them in situ. RESIRE experiments yielded flux-normalized respiration rates of 0.4 ± 0.1 d −1 at BATS when excluding an outlier of 1.52 d −1 , while these rates were undetectable along the WAP (0.01 ± 0.02 d −1 ). At BATS, flux-normalized respiration rates decreased exponentially with respect to depth below the euphotic zone with a 75% reduction between the 150 and 500 m depths. These findings provide quantitative and mechanistic insights into the processes that control the transfer efficiency of particle flux through the mesopelagic and its variability throughout the global oceans.
    Print ISSN: 0886-6236
    Electronic ISSN: 1944-9224
    Topics: Biology , Chemistry and Pharmacology , Geography , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
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    Revisiting carbon flux through the ocean's twilight zone (2007)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2007-04-28
    Description: The oceanic biological pump drives sequestration of carbon dioxide in the deep sea via sinking particles. Rapid biological consumption and remineralization of carbon in the "twilight zone" (depths between the euphotic zone and 1000 meters) reduce the efficiency of sequestration. By using neutrally buoyant sediment traps to sample this chronically understudied realm, we measured a transfer efficiency of sinking particulate organic carbon between 150 and 500 meters of 20 and 50% at two contrasting sites. This large variability in transfer efficiency is poorly represented in biogeochemical models. If applied globally, this is equivalent to a difference in carbon sequestration of more than 3 petagrams of carbon per year.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Buesseler, Ken O -- Lamborg, Carl H -- Boyd, Philip W -- Lam, Phoebe J -- Trull, Thomas W -- Bidigare, Robert R -- Bishop, James K B -- Casciotti, Karen L -- Dehairs, Frank -- Elskens, Marc -- Honda, Makio -- Karl, David M -- Siegel, David A -- Silver, Mary W -- Steinberg, Deborah K -- Valdes, Jim -- Van Mooy, Benjamin -- Wilson, Stephanie -- New York, N.Y. -- Science. 2007 Apr 27;316(5824):567-70.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. kbuesseler@whoi.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17463282" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Carbon/metabolism ; Carbon Dioxide ; Copepoda/physiology ; *Ecosystem ; Food Chain ; Geologic Sediments/chemistry ; Hydrogen-Ion Concentration ; Pacific Ocean ; Phytoplankton/physiology ; *Seawater/chemistry ; Zooplankton/physiology
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 6
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    Climate change. Will ocean fertilization work? (2003)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2003-04-05
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Buesseler, Ken O -- Boyd, Philip W -- New York, N.Y. -- Science. 2003 Apr 4;300(5616):67-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. kbuesseler@whoi.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12677048" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Biomass ; *Carbon Dioxide/metabolism ; *Iron ; Oceans and Seas ; Photosynthesis ; Phytoplankton/*growth & development/metabolism ; *Seawater ; Temperature
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 7
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    Global iron connections between desert dust, ocean biogeochemistry, and climate (2005)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2005-04-02
    Description: The environmental conditions of Earth, including the climate, are determined by physical, chemical, biological, and human interactions that transform and transport materials and energy. This is the "Earth system": a highly complex entity characterized by multiple nonlinear responses and thresholds, with linkages between disparate components. One important part of this system is the iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production. Here we review the key components of this cycle, identifying critical uncertainties and priorities for future research.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jickells, T D -- An, Z S -- Andersen, K K -- Baker, A R -- Bergametti, G -- Brooks, N -- Cao, J J -- Boyd, P W -- Duce, R A -- Hunter, K A -- Kawahata, H -- Kubilay, N -- laRoche, J -- Liss, P S -- Mahowald, N -- Prospero, J M -- Ridgwell, A J -- Tegen, I -- Torres, R -- New York, N.Y. -- Science. 2005 Apr 1;308(5718):67-71.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Environmental Sciences, University of East Anglia, Norwich NR47TJ, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/15802595" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Carbon Dioxide ; *Climate ; Desert Climate ; *Dust ; *Iron/metabolism ; Oceans and Seas ; Phytoplankton/physiology ; *Seawater ; Soil
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 8
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    Mesoscale iron enrichment experiments 1993-2005: synthesis and future directions (2007)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2007-02-03
    Description: Since the mid-1980s, our understanding of nutrient limitation of oceanic primary production has radically changed. Mesoscale iron addition experiments (FeAXs) have unequivocally shown that iron supply limits production in one-third of the world ocean, where surface macronutrient concentrations are perennially high. The findings of these 12 FeAXs also reveal that iron supply exerts controls on the dynamics of plankton blooms, which in turn affect the biogeochemical cycles of carbon, nitrogen, silicon, and sulfur and ultimately influence the Earth climate system. However, extrapolation of the key results of FeAXs to regional and seasonal scales in some cases is limited because of differing modes of iron supply in FeAXs and in the modern and paleo-oceans. New research directions include quantification of the coupling of oceanic iron and carbon biogeochemistry.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Boyd, P W -- Jickells, T -- Law, C S -- Blain, S -- Boyle, E A -- Buesseler, K O -- Coale, K H -- Cullen, J J -- de Baar, H J W -- Follows, M -- Harvey, M -- Lancelot, C -- Levasseur, M -- Owens, N P J -- Pollard, R -- Rivkin, R B -- Sarmiento, J -- Schoemann, V -- Smetacek, V -- Takeda, S -- Tsuda, A -- Turner, S -- Watson, A J -- New York, N.Y. -- Science. 2007 Feb 2;315(5812):612-7.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉National Institute for Water and Atmospheric Research (NIWA) Centre for Chemical and Physical Oceanography, Department of Chemistry, University of Otago, Dunedin, New Zealand. pboyd@alkali.otago.ac.nz〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17272712" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere ; Carbon/analysis/metabolism ; Carbon Dioxide ; Chlorophyll/analysis ; Climate ; Diatoms/growth & development ; *Ecosystem ; *Iron/analysis ; Oceans and Seas ; Phytoplankton/*growth & development/metabolism ; *Seawater ; Zooplankton/*growth & development
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 9
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    Comment on "The Southern Ocean biological response to aeolian iron deposition" (2008)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2008-01-12
    Description: Cassar et al. (Reports, 24 August 2007, p. 1067) proposed that aerosol-iron input enhances Southern Ocean export production. Their conclusion critically depends upon aerosol-iron modeling simulations not validated with iron-deposition data and dust dissolution rates based on Northern Hemisphere atmospheric chemical conditions (low pH). This diminishes the relevance of their findings and demonstrates that applying such models to this region is premature.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Boyd, Philip W -- Mackie, Douglas -- New York, N.Y. -- Science. 2008 Jan 11;319(5860):159; author reply 159. doi: 10.1126/science.1149884.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉National Institute of Water and Atmospheric Research Centre for Chemical and Physical Oceanography, Department of Chemistry, University of Otago, Dunedin, New Zealand. pboyd@alkali.otago.ac.nz〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18187641" target="_blank"〉PubMed〈/a〉
    Keywords: *Atmosphere ; Dust ; Iron/*analysis ; Models, Theoretical ; Oceans and Seas ; Phytoplankton/growth & development ; *Seawater/chemistry ; Wind
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 10
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    Environment. Ocean iron fertilization--moving forward in a sea of uncertainty (2008)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2008-01-12
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Buesseler, Ken O -- Doney, Scott C -- Karl, David M -- Boyd, Philip W -- Caldeira, Ken -- Chai, Fei -- Coale, Kenneth H -- de Baar, Hein J W -- Falkowski, Paul G -- Johnson, Kenneth S -- Lampitt, Richard S -- Michaels, Anthony F -- Naqvi, S W A -- Smetacek, Victor -- Takeda, Shigenobu -- Watson, Andrew J -- New York, N.Y. -- Science. 2008 Jan 11;319(5860):162. doi: 10.1126/science.1154305.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. kbuesseler@whoi.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18187642" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Carbon Dioxide/metabolism ; Climate ; Cost-Benefit Analysis ; *Ecosystem ; *Iron/metabolism ; Oceans and Seas ; Phytoplankton/*growth & development ; *Seawater/chemistry
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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