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| Open AccessEfficient dissolved organic carbon production and export in the oligotrophic ocean
The degree of regional variability in marine dissolved organic carbon (DOC) export production is poorly constrained on a global scale. Here, the authors combine an artificial neural network and a data-constrained ocean circulation model to show that the efficiency of DOC export varies 3-fold across regions.
- Saeed Roshan
- & Timothy DeVries
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Article
| Open AccessMethane- and dissolved organic carbon-fueled microbial loop supports a tropical subterranean estuary ecosystem
It remains unclear how oligotrophic habitats in subterranean estuaries sustain complex ecosystems. Here, using stable isotopic evidence from organic matter and pelagic shrimp, the authors show that a microbial loop fuelled by methane and dissolved organic carbon sustains the anchialine food web.
- D. Brankovits
- , J. W. Pohlman
- & B. Phillips
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| Open AccessThe molecular basis of phosphite and hypophosphite recognition by ABC-transporters
Some bacteria can use inorganic phosphite and hypophosphite as sources of inorganic phosphorus. Here, the authors report crystal structures of the periplasmic proteins that bind these reduced phosphorus species and show that a P-H…π interaction between the ligand and binding site determines their specificity.
- Claudine Bisson
- , Nathan B. P. Adams
- & Andrew Hitchcock
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Article
| Open AccessThe role of Atlantic overturning circulation in the recent decline of Atlantic major hurricane frequency
The reason for the decline in frequency of Atlantic major hurricanes since 2005 is still debated. Here the authors combine observations with model simulations to show that this decline is largely due to changes in the Atlantic ocean meridional overturning circulation.
- Xiaoqin Yan
- , Rong Zhang
- & Thomas R. Knutson
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| Open AccessMussel larvae modify calcifying fluid carbonate chemistry to promote calcification
The sensitivity of mussel larvae to ocean acidification, particularly during the time of shell formation, remains uncertain. Here, the authors show that larvae can elevate calcium carbonate saturation state beneath their shell to enhance calcification, but this ability is compromised by ocean acidification.
- Kirti Ramesh
- , Marian Y. Hu
- & Frank Melzner
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| Open AccessOcean forecasting of mesoscale features can deteriorate by increasing model resolution towards the submesoscale
The degree to which increasing the resolution of ocean models to consider submesoscale dynamics will improve prediction of mesoscale features remains uncertain. Here, via data assimilation experiments, the authors show higher resolution models do not necessarily provide improved dynamical solutions.
- Paul A. Sandery
- & Pavel Sakov
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Article
| Open AccessHolocene sea ice variability driven by wind and polynya efficiency in the Ross Sea
Strong regional heterogeneity prevents thorough understanding of the recent increase in Antarctic sea ice. Here, analysis of marine and ice cores in the Western Ross Sea shows that late Holocene contrasting sea ice patterns between open and coastal areas are related to katabatic winds and polynya efficiency.
- K. Mezgec
- , B. Stenni
- & M. Frezzotti
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| Open AccessPlanktic foraminifera form their shells via metastable carbonate phases
Understanding foraminifera mineralisation pathways is essential to correctly decipher the geochemical climate signals recorded in their shells. Here, the authors identify a non-classical crystallization pathway via metastable phases for Orbulina universa and Neogloboquadrina dutertrei.
- D. E. Jacob
- , R. Wirth
- & S. M. Eggins
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| Open AccessRecycled iron fuels new production in the eastern equatorial Pacific Ocean
In the eastern equatorial Pacific, upwelling supplies nitrate in excess of iron relative to phytoplankton requirements. Here, using nitrate isotopes, the authors show that iron recycling in surface waters supports nitrate consumption, lowering surface nitrate concentration and explaining its variation.
- Patrick A. Rafter
- , Daniel M. Sigman
- & Katherine R. M. Mackey
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| Open AccessMarine biogeographic realms and species endemicity
Global maps of biogeographic realms help to understand the geological and ecological processes that gave rise to species distributions, yet a marine realm map has been lacking. Here, Costello et al. use a database of over 65,000 species to reveal 30 marine biogeographic realms and high rates of species endemicity.
- Mark J. Costello
- , Peter Tsai
- & Chhaya Chaudhary
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| Open AccessCenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering
Reverse weathering reactions on or in the seafloor are a major sink of many elements and alkalinity in seawater. Here, the authors show how reduced rates of reverse weathering may be responsible for global cooling and increased seawater Mg/Ca over the past 50 million years.
- Ann G. Dunlea
- , Richard W. Murray
- & John A. Higgins
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Article
| Open AccessCascading effects of thermally-induced anemone bleaching on associated anemonefish hormonal stress response and reproduction
Elevated temperatures can cause anemones to bleach, with unknown effects on their associated symbiotic fish. Here, Beldade and colleagues show that climate-induced bleaching alters anemonefish hormonal stress response, resulting in decreased reproductive hormones and severely impacted reproduction.
- Ricardo Beldade
- , Agathe Blandin
- & Suzanne C. Mills
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| Open AccessSpringtime winds drive Ross Sea ice variability and change in the following autumn
Antarctic sea ice extent continues to increase, with autumn sea ice advances in the western Ross Sea particularly anomalous. Here, based on analysis of independent datasets, the authors show that springtime zonal winds in the high latitude South Pacific drive western Ross Sea autumn sea ice conditions.
- Marika M. Holland
- , Laura Landrum
- & Sharon Stammerjohn
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| Open AccessLate Neoproterozoic seawater oxygenation by siliceous sponges
The Ediacaran–Cambrian oxygenation of seawater is thought to have been caused by lifeforms engaging in ecosystem engineering. Here, the authors show that siliceous sponges increased seawater dissolved oxygen concentrations by redistributing organic carbon oxidation through filtering suspended organic matter.
- Michael Tatzel
- , Friedhelm von Blanckenburg
- & Dorothee Hippler
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| Open AccessThe onset of widespread marine red beds and the evolution of ferruginous oceans
The evolution of oceanic redox state in the past is poorly known. Here, the authors present a temporal record of banded iron formations and marine red beds, which indicate deep-ocean oxygenation occurred in the middle Ediacaran, coinciding with the onset of widespread marine red beds.
- Haijun Song
- , Ganqing Jiang
- & Chengshan Wang
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Article
| Open AccessRedox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
The potential contribution of redox reactions to acidification in coastal waters is unclear. Here, using measurements from the Chesapeake Bay, the authors show that pH minimum occurs at mid-depths where acids are produced via hydrogen sulfide oxidation in waters mixed upward from anoxic depths.
- Wei-Jun Cai
- , Wei-Jen Huang
- & W. Michael Kemp
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Article
| Open AccessVertical ocean heat redistribution sustaining sea-ice concentration trends in the Ross Sea
The mechanisms responsible for the overall expansion of Antarctic sea-ice in recent decades remain unclear. Here, using observations and model results, the authors show that ice-ocean feedbacks, triggered by an external perturbation, could be responsible for changes in sea-ice extent observed in the Ross Sea.
- Olivier Lecomte
- , Hugues Goosse
- & Violette Zunz
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| Open AccessLong-range transport of airborne microbes over the global tropical and subtropical ocean
The extent to which the ocean acts as a sink and source of airborne particles to the atmosphere is unresolved. Here, the authors report high microbial loads over the tropical Atlantic, Pacific and Indian oceans and propose islands as stepping stones for the transoceanic transport of terrestrial microbes..
- Eva Mayol
- , Jesús M. Arrieta
- & Carlos M. Duarte
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| Open AccessSpiraling pathways of global deep waters to the surface of the Southern Ocean
Deep waters of the Atlantic, Pacific and Indian Oceans upwell in the Southern Oceanbut the exact pathways are not fully characterized. Here the authors present a three dimensional view showing a spiralling southward path, with enhanced upwelling by eddy-transport at topographic hotspots.
- Veronica Tamsitt
- , Henri F. Drake
- & Wilbert Weijer
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| Open AccessSediment transport drives tidewater glacier periodicity
The reason some of the Earth’s tidewater glaciers are advancing despite increasing temperatures is not entirely clear. Here, using a numerical model that simulates both ice and sediment dynamics, the authors show that internal dynamics drive glacier variability independent of climate.
- Douglas Brinkerhoff
- , Martin Truffer
- & Andy Aschwanden
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| Open AccessThe unprecedented 2015/16 Tasman Sea marine heatwave
The Tasman Sea experienced an unprecedented marine heatwave in 2015/16, with important ecological impacts. Oliveret al. link this event to warm, southwards flowing waters from East Australia and find that climate change has made these events almost seven times more likely.
- Eric C. J. Oliver
- , Jessica A. Benthuysen
- & Sarah E. Perkins-Kirkpatrick
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| Open AccessRadiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2
Establishing the efficiency of the biological carbon pump is needed to constrain the impact of ocean circulation on the carbon cycle. Here, the authors compile a global array of ocean–atmosphere radiocarbon disequilibrium estimates and evaluate the strength of the carbon pump over the last glacial maximum.
- L. C. Skinner
- , F. Primeau
- & A. E. Scrivner
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Editorial
| Open AccessRising to the challenge of surging seas
Amid increasingly extreme projections for future sea-level rise, concerns are mounting that policymakers are struggling to keep abreast of fast-paced scientific developments. To ease this burden and increase the accessibility of published research, we have compiled an editor-curated collection of the most recent sea-level rise articles published at Nature Communications.
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| Open AccessGlobal mismatch between fishing dependency and larval supply from marine reserves
The effectiveness of marine reserves relies on whether they supply substantial recruitment outside their boundaries. Here, Andrello and colleagues use models of larval fish dispersal to show that countries most dependent on coastal fisheries receive the lowest larval supplies from marine reserves.
- Marco Andrello
- , François Guilhaumon
- & David Mouillot
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| Open AccessWestern tropical Pacific multidecadal variability forced by the Atlantic multidecadal oscillation
The western tropical Pacific is a main source of heat and moisture for the global atmosphere, yet the mechanism for the multidecadal sea surface temperature variability in this region remains unknown. Here, the authors show that this variability is forced by the remote Atlantic multidecadal oscillation
- Cheng Sun
- , Fred Kucharski
- & Ruiqiang Ding
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| Open AccessGreening of the Sahara suppressed ENSO activity during the mid-Holocene
Evolution of the El Niño-Southern Oscillation through the Holocene remains uncertain. Here, via fully coupled model simulations, the authors show that increased Saharan vegetation and reduced dust emissions 6 kyr BP significantly affect ENSO variability through changes in the West African Monsoon strength.
- Francesco S. R. Pausata
- , Qiong Zhang
- & Zhengyu Liu
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| Open AccessUnderstanding extreme sea levels for broad-scale coastal impact and adaptation analysis
Uncertainties in contemporary extreme sea levels (ESL) from mean sea level rise (SLR) projections have been overlooked in broad-scale risk and adaptation studies. Here, the authors quantify the uncertainties in present-day global ESL estimates and find that they exceed those from global SLR projections.
- T. Wahl
- , I. D. Haigh
- & A. B. A. Slangen
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| Open AccessMarine viruses discovered via metagenomics shed light on viral strategies throughout the oceans
The understanding of marine virus diversity and function is in its infancy. Here, Coutinhoet al. assemble a data set of new viral contigs and use co-occurrence analyses to identify the putative hosts, elucidate infection strategies and viral strategies for exploiting their hosts.
- Felipe H. Coutinho
- , Cynthia B. Silveira
- & Fabiano L. Thompson
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| Open AccessSkillful prediction of northern climate provided by the ocean
The degree to which ocean heat is imprinted on the atmosphere and can be used to predict climate remains unclear. Here, the authors demonstrate skillful observation-based prediction of northwestern European and Arctic climate from upstream sea surface temperature anomalies in the subpolar North Atlantic.
- Marius Årthun
- , Tor Eldevik
- & Noel S. Keenlyside
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| Open AccessEvidence for fungal and chemodenitrification based N2O flux from nitrogen impacted coastal sediments
Predicting nitrous oxide emissions (N2O) remains difficult due to the numerous N2O production pathways. Here, the authors use incubations simulating high nitrate inputs to show that, in intertidal sediments, increases in N2O flux are largely mediated by fungal denitrification and/or chemodenitrification.
- Scott D. Wankel
- , Wiebke Ziebis
- & Karsten Zengler
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| Open AccessRecent enhancement of central Pacific El Niño variability relative to last eight centuries
El Niño events in the Central Pacific may be changing due to climate change, but long records to support this are lacking. Here, the authors present sea surface temperature reconstructions from tree cellulose for the last 800 years which suggest the variability of Central Pacific El Niño events has increased.
- Yu Liu
- , Kim M. Cobb
- & Hans W. Linderholm
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| Open AccessIron limitation of microbial phosphorus acquisition in the tropical North Atlantic
The influence iron exerts over the acquisition of dissolved organic phosphorus in regions of the oceans co-limited by nitrogen and phosphorus is poorly constrained. Here, the authors demonstrate enhanced alkaline phosphatase activity of natural marine microbial communities following iron fertilization.
- T. J. Browning
- , E. P. Achterberg
- & C. M. Moore
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| Open AccessPicocyanobacteria and deep-ocean fluorescent dissolved organic matter share similar optical properties
The sources of marine chromophoric dissolved organic matter and associated fluorescent DOM (FDOM) remain unclear. Here, the authors demonstrate that picocyanobacteria release FDOM similar to typical fluorescent signals found in the ocean, and are likely to be an important source of marine FDOM.
- Zhao Zhao
- , Michael Gonsior
- & Feng Chen
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| Open AccessLink between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei
The degree to which the diurnal light/dark cycle influences Mg-heterogeneity in foraminifera with complex shell morphologies remains unknown. Here, using highly spatially resolved analytical techniques, the authors investigate Mg-banding and calcification in isotope-labelledNeogloboquadrina dutertreispecimens.
- Jennifer S. Fehrenbacher
- , Ann D. Russell
- & Pamela Martin
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| Open AccessDispersion/dilution enhances phytoplankton blooms in low-nutrient waters
The degree to which horizontal transport affects phytoplankton ecosystems remains understudied. Here, the authors combine satellite observations, ARGO float data and a simple ecosystem model to explore the impact of horizontal stirring on naturally-stimulated fine-scale phytoplankton blooms.
- Yoav Lehahn
- , Ilan Koren
- & Emmanuel Boss
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| Open AccessA coupled human-Earth model perspective on long-term trends in the global marine fishery
Global marine fish harvest increased over the 20th century, reaching a peak in the 1990s. Here, Galbraith and colleagues analyse a model combining both ecological and economic drivers to weigh the factors most likely to contribute to long-term changes in fish harvests.
- E. D. Galbraith
- , D. A. Carozza
- & D. Bianchi
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| Open AccessRemineralization of particulate organic carbon in an ocean oxygen minimum zone
The downward transfer of organic carbon from the surface to the deep ocean is increased in oxygen minimum zones relative to oxic waters. Here, the authors show reduced interactions of zooplankton with sinking particles owing to low oxygen are likely the primary reason for the observed high transfer of carbon.
- E. L. Cavan
- , M. Trimmer
- & R. Sanders
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| Open AccessEnhanced biennial variability in the Pacific due to Atlantic capacitor effect
Biennial variability has intensified in the Pacific in recent decades, but the cause of this increase is not fully understood. Here, with statistical analyses and numerical experiments, the authors show that an Atlantic capacitor effect has given rise to this enhanced biennial variability since the early 1990s.
- Lei Wang
- , Jin-Yi Yu
- & Houk Paek
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| Open AccessRapid emergence of climate change in environmental drivers of marine ecosystems
Climate change is expected to alter ocean ecology, and to potentially impact the ecosystem services provided to humankind. Here, the authors address how rapidly multiple factors that affect marine ecosystems are likely to develop in the future ocean and the remedial effects climate mitigation might have.
- Stephanie A. Henson
- , Claudie Beaulieu
- & Jorge L. Sarmiento
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| Open AccessTopographic enhancement of vertical turbulent mixing in the Southern Ocean
Turbulent mixing next to rough topographic features is believed to be key in the closure of the abyssal ocean circulation. Here, using Southern Ocean data, the authors show that mixing hotspots trap fluid and mix it for long periods, explaining the global impact of relatively few mixing hotspots.
- A. Mashayek
- , R. Ferrari
- & A. Naveira Garabato
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| Open AccessMechanisms driving variability in the ocean forcing of Pine Island Glacier
Pine Island Glacier terminates in a rapidly melting ice shelf and ocean conditions are believed to influence its contribution to sea level rise. Here, the authors show that variability in these ocean conditions is driven by a combination of changes in ocean circulation and local surface heat fluxes.
- Benjamin G. M. Webber
- , Karen J. Heywood
- & Tae Wan Kim
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| Open AccessAbrupt cooling over the North Atlantic in modern climate models
Concerns on climate change include the risk of abrupt cooling in the North Atlantic. Here, the authors analyse CMIP5 projections and show that a convection collapse in the subpolar gyre can cool this region by up to 3°C in 10 years, which is as likely to occur by 2100 as a continuous warming.
- Giovanni Sgubin
- , Didier Swingedouw
- & Amine Bennabi
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| Open AccessExtreme oceanographic forcing and coastal response due to the 2015–2016 El Niño
ENSO end members El Niño and La Niña are linked to elevated coastal hazards across the Pacific region. Here, the authors show that the wave conditions and coastal response for the 2015–16 El Niño indicate that it was one of the most significant events of the last 145 years.
- Patrick L. Barnard
- , Daniel Hoover
- & Katherine A. Serafin
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| Open AccessBacterial community dynamics are linked to patterns of coral heat tolerance
Coral-associated microbes could enhance the capacity of their host organism to respond to environmental change. Ziegler and colleagues use a reciprocal transplant experiment to show that microbiomes of heat-tolerant corals are more resilient to change than those of heat-sensitive corals.
- Maren Ziegler
- , Francois O. Seneca
- & Christian R. Voolstra
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| Open AccessMismatch between marine plankton range movements and the velocity of climate change
Marine plankton are the basis of the oceanic food chain. Here, Chivers and colleagues use ocean-basin wide plankton population data over six decades to show huge differences in the response of different plankton groups to climate change with major implications for the marine ecosystem and fisheries.
- William J. Chivers
- , Anthony W. Walne
- & Graeme C. Hays
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| Open AccessIce sheets as a missing source of silica to the polar oceans
Glacial runoff often has relatively low dissolved silica concentrations and therefore ice sheets have been thought insignificant in the global silicon cycle. Here, the authors show that ice sheets likely play an important role in the production and export of dissolved and dissolvable amorphous silica downstream.
- Jon R. Hawkings
- , Jemma L. Wadham
- & Rob Raiswell
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| Open AccessA swarm of autonomous miniature underwater robot drifters for exploring submesoscale ocean dynamics
Observing dynamics associated with oceanic submesoscales requires simultaneous sampling at multiple locations. Here, the authors show that a swarm of 16 Mini-Autonomous Underwater Explorers (M-AUEs), whose 3D trajectories are measured near-continuously, can resolve features of the flow at these scales.
- Jules S. Jaffe
- , Peter J. S. Franks
- & Adrien Boch
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| Open AccessSynchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific
Potential age model problems with marine Δ14C records have obscured our understanding of the role of the deep-ocean in deglacial atmospheric CO2rise. Here, the authors show that deglacial ventilation of EEP thermocline and deep waters occurred synchronously and was coeval with changes in Atlantic records.
- Natalie E. Umling
- & Robert C. Thunell
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| Open AccessPrehistorical and historical declines in Caribbean coral reef accretion rates driven by loss of parrotfish
Fishing of keystone herbivores such as parrotfish is thought to negatively impact corals. Here, Cramer and colleagues analyse the sedimentary record for the last 3,000 years from three coral reef sites in the Caribbean and show that indeed coral declines are linked to parrotfish declines.
- Katie L. Cramer
- , Aaron O’Dea
- & Richard D. Norris