6/06/2013

NATURE, SCIENCE, GEOLOGY, NATURE GEOSCIENCE May 28 - June 4


NATURE

1. Japan aims high for growth
Innovation in science is at the heart of government plans to boost the economy.
David Cyranoski

The reform platform includes a new growth strategy, and central to that strategy is innovation in science and technology. Abe’s cabinet has already committed hundreds of billions of yen to space, physics and stem-cell research to recuperate the loss of the competitive edge it once had over China, South Korea and other Asian rivals. It calls for 30% of new recruits at research institutes and universities to be female by 2016. And faced with fewer university graduates and a shrinking birth rate, Japan is looking to open itself up to foreigners. Under the plan, international researchers would occupy 30% of staff positions at leading research organizations by 2030.

2. Evolutionary dichotomy for rocky planets
Linda T. Elkins-Tanton
Nature 497, 570–572 (30 May 2013) doi:10.1038/497570a

Rocky planets that form and solidify close to their host stars may receive enough heat from the star to slow cooling, allowing time for water to escape into space and causing the planet to dry out. Rocky planets that form farther from their stars, beyond a critical distance, would cool quickly, trapping water in silicate minerals in their interiors and as liquid on their surfaces.
  
3. Palaeoanthropology: Hesitation on hominin history
William H. Kimbel
Nature 497, 573–574 (30 May 2013) doi:10.1038/497573a

Extensive studies of fossil skeletons of Australopithecus sediba provide fascinating details of the anatomy of this hominin species, but do not convincingly indicate its position on the evolutionary route to modern humans.

Sharon S. Hoffmann, Jerry F. McManus, William B. Curry & L. Susan Brown-Leger
Nature 497, 603–606 (30 May 2013) doi:10.1038/nature12145

Ratios of the radionuclides thorium-230 and protactinium-231 in sediment record ongoing export of 231Pa from the deep central Arctic Ocean and may indicate continuous deep-water exchange between the Arctic and Atlantic oceans throughout the past 35,000 years.

Keiko Hamano, Yutaka Abe & Hidenori Genda
Nature 497, 607–610 (30 May 2013) doi:10.1038/nature12163

Terrestrial planets can be divided into two distinct types on the basis of their evolutionary history during solidification from their initial molten state: type I planets (such as Earth) solidify within several million years and retain most of their water, and type II planets (possibly such as Venus), formed inside a critical distance, are desiccated by hydrodynamic escape.

Nancy J. Stevens, Erik R. Seiffert, Patrick M. O’Connor, Eric M. Roberts, Mark D. Schmitz+ et al.
Nature 497, 611–614 (30 May 2013) doi:10.1038/nature12161

7. Long-term warming restructures Arctic tundra without changing net soil carbon storage
Seeta A. Sistla, John C. Moore, Rodney T. Simpson, Laura Gough, Gaius R. Shaver+ et al.
Nature 497, 615–618 (30 May 2013) doi:10.1038/nature12129

Two decades of summer warming in an Alaskan tundra ecosystem increased plant biomass and woody dominance, indirectly increased winter soil temperature, homogenized the soil trophic structure and suppressed surface-soil-decomposer activity, but did not change net soil carbon or nitrogen storage.


SCIENCE

8. Radiation Will Make Astronauts' Trip to Mars Even Riskier
Richard A. Kerr
Science 31 May 2013: 1031.[DOI:10.1126/science.340.6136.1031]

Future astronauts headed for the Red Planet will have more than an imagined martian jinx to worry about: deep space radiation.

9. What Are Climate Models Missing?
Bjorn Stevens and Sandrine Bony
Science 31 May 2013: 1053-1054.[DOI:10.1126/science.1237554]

A better representation of the coupling between atmospheric water and circulation is necessary to reduce imprecision in climate model projections. 


10. Pebbles on Mars
Douglas J. Jerolmack
Science 31 May 2013: 1055-1056.[DOI:10.1126/science.1239343] 



The observation of conglomerates by the Mars rover Curiosity provides the most definitive proof yet of ancient river flow.

11. Measurements of Energetic Particle Radiation in Transit to Mars on the Mars Science Laboratory
C. Zeitlin, D. M. Hassler, F. A. Cucinotta, B. Ehresmann, R. F. Wimmer-Schweingruber, D. E. Brinza, S. Kang, G. Weigle, S. Böttcher, E. Böhm, S. Burmeister, J. Guo, J. Köhler, C. Martin, A. Posner, S. Rafkin, and G. Reitz
Science 31 May 2013: 1080-1084.[DOI:10.1126/science.1235989]

The radiation dose on a round-trip to Mars could represent a large fraction of the accepted lifetime limit for astronauts.


PNAS

12. Energetic basis of catalytic activity of layered nanophase calcium manganese oxides for water oxidation
Nancy Birkner, Sara Nayeri, Babak Pashaei, Mohammad Mahdi Najafpour, William H. Casey, and Alexandra Navrotsky
PNAS 2013 110 (22) 8801-8806, doi:10.1073/pnas.1306623110

13. Influence of organic films on the evaporation and condensation of water in aerosol
James F. Davies, Rachael E. H. Miles, Allen E. Haddrell, and Jonathan P. Reid
PNAS 2013 110 (22) 8807-8812; published ahead of print May 14, 2013, doi:10.1073/pnas.1305277110

14. High regional climate sensitivity over continental China constrained by glacial-recent changes in temperature and the hydrological cycle
Robert A. Eagle, Camille Risi, Jonathan L. Mitchell, John M. Eiler, Ulrike Seibt, J. David Neelin, Gaojun Li, and Aradhna K. Tripati
PNAS 2013 110 (22) 8813-8818; published ahead of print May 13, 2013, doi:10.1073/pnas.1213366110 

                                           
182Hf–182W age dating of a 26Al-poor inclusion and implications for the origin of short-lived radioisotopes in the early Solar System
Jesper C. Holst, Mia B. Olsen, Chad Paton, Kazuhide Nagashima, Martin Schiller, Daniel Wielandt, Kirsten K. Larsen, James N. Connelly, Jes K. Jørgensen, Alexander N. Krot, Åke Nordlund, and Martin Bizzarro
PNAS 2013 110 (22) 8819-8823; published ahead of print May 13, 2013, doi:10.1073/pnas.1300383110

15. Millennial-scale isotope records from a wide-ranging predator show evidence of recent human impact to oceanic food webs
Anne E. Wiley, Peggy H. Ostrom, Andreanna J. Welch, Robert C. Fleischer, Hasand Gandhi, John R. Southon, Thomas W. Stafford, Jr., Jay F. Penniman, Darcy Hu, Fern P. Duvall, and Helen F. James
PNAS 2013 110 (22) 8972-8977; published ahead of print May 13, 2013, doi:10.1073/pnas.1300213110

16. Benefit of pulsation in soft corals
Maya Kremien, Uri Shavit, Tali Mass, and Amatzia Genin
PNAS 2013 110 (22) 8978-8983; published ahead of print April 22, 2013, doi:10.1073/pnas.1301826110

17. Functional ecology of an Antarctic Dry Valley
Yuki Chan, Joy D. Van Nostrand, Jizhong Zhou, Stephen B. Pointing, and Roberta L. Farrell
PNAS 2013 110 (22) 8990-8995; doi:10.1073/pnas.1300643110


NATURE COMMUNICATIONS

Julie A. Bowles, Mike J. Jackson, Thelma S. Berquó, Peter A. Sølheid, Jeffrey S. Gee
28 May 2013 doi: 10.1038/ncomms2938

Cation ordering in cubic-structured oxides can strongly affect magnetic properties. Here, the authors show that in some natural titanomagnetites, large and reversible changes in Curie temperature result from annealing at moderate temperatures (350–400 °C), most likely arising from changes in cation ordering.


NATURE GEOSCIENCE

19. Palaeoclimate: When the dust settles
Eun Young Kwon & Eric D. Galbraith
Nature Geoscience 6, 423–424 (2013) doi:10.1038/ngeo1838

The amount of carbon stored in the deep ocean varied over glacial–interglacial cycles. Southern Ocean sediments from the past 360,000 years show that carbon storage also fluctuated within glacial periods, in concert with the fertilization of the Southern Ocean by wind-borne dust.


20. The amount of carbon stored in the deep ocean varied over glacial–interglacial cycles. Southern Ocean sediments from the past 360,000 years show that carbon storage also fluctuated within glacial periods, in concert with the fertilization of the Southern Ocean by wind-borne dust.

21. Plants, clouds and climate
Nature Geoscience 6, 413 (2013) doi:10.1038/ngeo1852
Published online 30 May 2013

Plant–cloud interactions have the potential to both cool and warm the climate. Ascertaining how these processes balance out at the global scale will require close collaboration between climate scientists and plant biologists.

22. Projectile remnants in central peaks of lunar impact craters
Z. Yue, B. C. Johnson, D. A. Minton, H. J. Melosh, K. Di, W. Hu & Y. Liu
Nature Geoscience 6, 435–437 (2013) doi:10.1038/ngeo1828

Unusual minerals observed in lunar craters were thought to originate from beneath the Moon's surface. Numerical simulations show that rather than being vaporized, much of the impactor material can survive in the crater, implying that the unusual minerals come from the impactor and may not be indigenous to the Moon.

23. Hydrogen generation from low-temperature water–rock reactions
L. E. Mayhew, E. T. Ellison, T. M. McCollom, T. P. Trainor & A. S. Templeton
Nature Geoscience 6, 478–484 (2013) doi:10.1038/ngeo1825

Hydrogen is commonly produced during the high-temperature hydration of mafic and ultramafic rocks. Laboratory experiments suggest that water–rock reactions also generate hydrogen at lower temperatures, potentially fuelling microbial life in ultramafic aquifers in oceanic and terrestrial crust.

24. Graphite formation by carbonate reduction during subduction
Matthieu E. Galvez, Olivier Beyssac, Isabelle Martinez, Karim Benzerara, Carine Chaduteau, Benjamin Malvoisin & Jacques Malavieille
Nature Geoscience 6, 473–477 (2013) doi:10.1038/ngeo1827

Carbon is carried into the Earth at subduction zones. Geochemical analysis of subducted sediments now exhumed in Alpine Corsica, France, reveal the formation of graphite during shallow subduction, implying that carbonate transformation to graphite aids transport into the deeper Earth.

25. A combination mode of the annual cycle and the El Niño/Southern Oscillation
Malte F. Stuecker, Axel Timmermann, Fei-Fei Jin, Shayne McGregor & Hong-Li Ren
Nature Geoscience (2013) doi:10.1038/ngeo1826

The development and termination of El Niño events seem to be coupled with the seasonal cycle. Statistical analyses suggest that this link reflects the presence of a combination climate mode with periods of 10 and 15 months.

26. The effect of sea level on glacial Indo-Pacific climate
Pedro N. DiNezio & Jessica E. Tierney
Nature Geoscience 6, 485–491 (2013) doi:10.1038/ngeo1823

The Indo-Pacific warm pool is the largest source of heat and moisture vapour to the atmosphere. Proxy reconstructions and model simulations suggest that during the Last Glacial Maximum, the exposure of the Sunda Shelf of Southeast Asia weakened deep convection over the warm pool.

27. Energy budget constraints on climate response

Alexander Otto, Friederike E. L. Otto,       Olivier Boucher, John Church, Gabi Hegerl, Piers M. Forster, Nathan P. Gillett, Jonathan Gregory, Gregory C. Johnson, Reto Knutti, Nicholas Lewis, Ulrike Lohmann,   Jochem Marotzke, Gunnar Myhre, Drew Shindell, Bjorn Stevens & Myles R. Allen
Nature Geoscience 6, 415–416 (2013) doi:10.1038/ngeo1836

The rate of climate warming has been lower than expected over the past decade. Energy budget considerations suggest that this does not significantly change estimates of the eventual (equilibrium) temperature rise in response to doubled atmospheric CO2 concentrations; the immediate temperature response to rising levels of greenhouse gases in the atmosphere – before an equilibrium is reached – may, however, need to be revised downwards.