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| Open AccessTwo centuries of limited variability in subtropical North Atlantic thermocline ventilation
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
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Silver hake tracks changes in Northwest Atlantic circulation
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
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Article
| Open AccessSouth China Sea hydrological changes and Pacific Walker Circulation variations over the last millennium
Tropical Pacific hydrology affects the global climate through the strength of the Pacific Walker Circulation. Yanet al. reconstruct variations in the Pacific Walker Circulation in the South China Sea over the last millennium and find that less precipitation fell during warmer and more rainfall during cool periods.
- Hong Yan
- , Liguang Sun
- & Wenhan Cheng
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Article
| Open AccessMapping the evolving strain field during continental breakup from crustal anisotropy in the Afar Depression
The spatial and temporal scales over which continental breakup occurs by mechanical deformation and magma intrusion remain controversial. Keiret al. quantify anisotropy across the Afar Triple Junction using S-wave splitting from earthquakes to evaluate the strain in a region of continental breakup.
- Derek Keir
- , M. Belachew
- & J.V. Rowland
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Coastal pollution limits pelagic larval dispersal
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
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Growth rates of Florida corals from 1937 to 1996 and their response to climate change
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
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Article
| Open AccessMultiple S-isotopic evidence for episodic shoaling of anoxic water during Late Permian mass extinction
A final catastrophe killed 90% of marine species at the end of the Permian period, but significant biodiversity loss preceded this event. In this study, sulphur isotope evidence suggests that incursion of anoxic water into shallow regions may have contributed to biodiversity loss.
- Yanan Shen
- , James Farquhar
- & Boswell A. Wing
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| Open AccessTracking the Atlantic Multidecadal Oscillation through the last 8,000 years
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
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Impact of the Mertz Glacier Tongue calving on dense water formation and export
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
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Evidence for infragravity wave-tide resonance in deep oceans
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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Deep-sea hydrothermal vent animals seek cool fluids in a highly variable thermal environment
Many animals adapt their behaviour according to their surroundings. Here, Bateset al.show that animals living in deep-sea hydrothermal vents choose habitats within their thermal limits.
- Amanda E Bates
- , Raymond W Lee
- & Miles D Lamare