Ocean sciences articles within Nature Communications

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  • Article
    | Open Access

    The dissolution of iron from sediments along ocean margins may stimulate photosynthesis and moderate global climate. This study shows how margin sediments supply iron in varying amounts between regions, and by distinct mechanisms, which may be due to geological characteristics and hydrological controls on land.

    • William B. Homoky
    • , Seth G. John
    •  & Rachel A. Mills

  • Article |

    Patchiness in the distribution of phytoplankton promotes many of the ecological interactions that underpin the marine food web. This study shows that turbulence, ubiquitous in the ocean, counter-intuitively ‘unmixes’ a population of motile phytoplankton, generating intense, small-scale patchiness in its distribution.

    • William M. Durham
    • , Eric Climent
    •  & Roman Stocker

  • Article |

    Iron plays a key role in controlling biological production in the Southern Ocean, yet mechanisms regulating iron availability are not completely understood. Here, Ingall et al.show that structural incorporation of reduced, organic iron into biogenic silica represents a new and substantial removal pathway.

    • Ellery D. Ingall
    • , Julia M. Diaz
    •  & Jay A. Brandes

  • Article
    | Open Access

    The abrupt ending of the Younger Dryas cooling episode marked the onset of the present interglacial and was the most prominent climate change in the Earth’s recent history. This study shows evidence for a sequence of events with a leading role of the ocean at the transition into the present day warm Holocene epoch.

    • Christof Pearce
    • , Marit-Solveig Seidenkrantz
    •  & Søren M. Kristiansen

  • Article
    | Open Access

    The branched inflow of warm Atlantic Water to the Arctic has been known for more than a hundred years, yet what controls the relative strengths of the two pathways remains poorly understood. Here, the authors identify the role of atmospheric circulation over the northern Barents Sea in controlling inflow.

    • Vidar S. Lien
    • , Frode B. Vikebø
    •  & Øystein Skagseth

  • Article
    | Open Access

    Active seafloor spreading has been documented in some of the tectonically active basins of the Gulf of California. This work presents new geophysical and geochemical data as evidence that active seafloor spreading is also occurring in the northernmost Wagner and Consag basins of the Gulf.

    • Rosa Ma Prol-Ledesma
    • , Marco-Antonio Torres-Vera
    •  & Carlos Robinson

  • Article
    | Open Access

    Palaeoclimate proxies, such as shells, record past ocean changes. A radiocarbon study based on a shell chronology from the Icelandic shelf is used to track changes in ocean circulation and climate for the past 1,350 years, suggesting a declining influence of North Atlantic surface waters on the Icelandic shelf over the last millennium.

    • Alan D. Wanamaker Jr
    • , Paul G. Butler
    •  & Christopher A. Richardson

  • Article |

    Small-scale ocean dynamics can have wide reaching impacts on the larger-scale ocean circulation. Using temperature and velocity data, this study shows the presence of abyssal vortices in the Eastern Mediterranean basin, adding complexity to the structure and evolution of water masses in this region.

    • A. Rubino
    • , F. Falcini
    •  & A. Capone

  • Article
    | Open Access

    The calving of the Mertz Glacier occurred in 2010 in East Antarctica, brought on by the re-positioning of a large iceberg. Using satellite data, this study shows a reduction in sea ice production following the calving, interpreted as a potential regime shift towards reduced sea ice production for the coming decades.

    • T. Tamura
    • , G.D. Williams
    •  & K.I. Ohshima

  • Article
    | Open Access

    Ocean circulation moves heat and gases between the ocean and atmosphere, impacting the carbon cycle at decadal timescales. Here, a radiocarbon coral record of ocean mixing from Bermuda suggests that the formation of mode water, and thus carbon uptake, have been more stable over the past 200 years than previously thought.

    • Nathalie F. Goodkin
    • , Ellen R. M. Druffel
    •  & Scott C. Doney

  • Article |

    Many organisms are responding to a warming climate by shifts in spatial distribution. The poleward movement of silver hake,Merluccius bilinearis, over the last forty years is related to the position of the Gulf Stream and Atlantic meridional overturning circulation through changes in local bottom water temperature.

    • Janet A. Nye
    • , Terrence M. Joyce
    •  & Jason S. Link

  • Article |

    Storm water runoff and wastewater effluent are discharged into oceans, but the full ecological effects of these discharges are unknown. Here, the authors examine the population structure of a marine organism, the bat star, and show that these discharges alter the genetic structure and larval dispersal of this species.

    • Jonathan B. Puritz
    •  & Robert J. Toonen

  • Article |

    Ocean acidification due to increasing carbon dioxide levels can affect the growth and viability of corals. In this study, the authors measured extension, calcification and density in Florida corals collected in 1996, and show that recent climate change did not cause a decline in their extension or calcification.

    • Kevin P. Helmle
    • , Richard E. Dodge
    •  & C. Mark Eakin

  • Article
    | Open Access

    The origin of the Atlantic Multidecadal Oscillation, a semi-periodic variability of sea-surface temperature, is unknown. Knudsenet al.show that 55- to 70-year climate oscillations existed throughout the last 8,000 years, suggesting that the Atlantic Multidecadal Oscillation is a permanent feature of the Holocene climate induced by internal ocean variability.

    • Mads Faurschou Knudsen
    • , Marit-Solveig Seidenkrantz
    •  & Antoon Kuijpers

  • Article |

    Antarctic bottom water is important for the global climate system, but its main source in East Antarctica was altered recently because of calving of the Mertz Glacier Tongue. The authors model this event and find large changes in dense water exports from the region.

    • Kazuya Kusahara
    • , Hiroyasu Hasumi
    •  & Guy D. Williams

  • Article |

    Ocean tides and infragravity waves—the Earths 'hum'—have very different periods and wavelengths. Sugioka and colleagues report resonance between these two phenomena using arrays of broadband ocean-bottom seismometers and show that some tidal energy is transferred to the deep oceans through this coupling.

    • Hiroko Sugioka
    • , Yoshio Fukao
    •  & Toshihiko Kanazawa

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