News & Views |
Featured
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News & Views |
Climate swings in extinction
Extreme temperature swings and deteriorating environments are perhaps what killed most life in the end-Permian extinction, suggest climate model simulations. Siberian Traps volcanism probably triggered the events.
- Ying Cui
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News & Views |
Enriched carbon source detected
Estimates of carbon in the deep mantle vary by more than an order of magnitude. Coupled volcanic CO2 emission data and magma supply rates reveal a carbon-rich mantle plume source region beneath Hawai'i with 40% more carbon than previous estimates.
- Peter H. Barry
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Editorial |
More space for space
Born from astronomy, the study of planets is becoming increasingly geoscience. As divisions between disciplines continue to blur in Solar System studies, at Nature Geoscience we are looking forward to exciting joint projects with Nature Astronomy.
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Progress Article |
Impact bombardment of the terrestrial planets and the early history of the Solar System
About 4 billion years ago, the terrestrial planets were bombarded by asteroids following an orbital shake-up of the outer Solar System. Lunar samples, planetary cratering records and dynamical models piece together an increasingly coherent view of this bombardment interval.
- Caleb I. Fassett
- & David A. Minton
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Letter |
Layered convection as the origin of Saturn’s luminosity anomaly
Saturn is brighter than expected for a gas giant of its age. Calculations of Saturn’s thermal evolution show that the presence of layered convection in Saturn’s interior—much like that observed in the Earth’s oceans—would have slowed the planet’s cooling and may explain Saturn’s anomalous luminosity.
- Jérémy Leconte
- & Gilles Chabrier
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Article |
High-velocity collisions from the lunar cataclysm recorded in asteroidal meteorites
Lunar samples suggest that the inner Solar System was bombarded by asteroids about 4 Gyr ago. Radiometric ages of meteorites suggest an unusual number of high-velocity asteroids at this time, consistent with a dynamical origin of the bombardment in which the asteroids were pushed by outer planet migration onto highly eccentric orbits.
- S. Marchi
- , W. F. Bottke
- & C. T. Russell
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Letter |
A chaotic long-lived vortex at the southern pole of Venus
A whirling vortex has been observed in the atmosphere at the south pole of Venus. Cloud motions tracked by the Venus Express spacecraft suggest that the south polar vortex is long-lived, erratic and baroclinic in character.
- I. Garate-Lopez
- , R. Hueso
- & P. Drossart
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Commentary |
Abandoned frontier
Over the past fifty years, NASA has pushed the frontiers of science and exploration to the edges of our Solar System. Declining funding for research and robotic missions may leave planetary exploration unfinished and young scientists stranded.
- Paul O. Hayne
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Editorial |
Expanding spheres of interest
Extrasolar planet research is booming. We welcome submissions with links to the geosciences.
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Commentary |
Strange news from other stars
The dawn of exoplanet discovery has unearthed a rich tapestry of planets different from anything encountered in the Solar System. Geoscientists can and should be in the vanguard of investigating what is out there in the Universe.
- Raymond T. Pierrehumbert
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News & Views |
Rising sulphur on Venus
Thirty years ago, the spacecraft Pioneer Venus observed the peak and decline of sulphur dioxide levels above Venus's clouds. Similar observations by Venus Express reveal a surprisingly variable venusian atmosphere.
- Larry W. Esposito
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Letter |
Variations of sulphur dioxide at the cloud top of Venus’s dynamic atmosphere
A pulse of sulphur dioxide in Venus’s upper atmosphere was observed by the Pioneer Venus spacecraft in the 1970s and 1980s and attributed to volcanism. Recent sulphur dioxide measurements from Venus Express indicate decadal-scale fluctuations in sulphur dioxide above Venus’s cloud tops in an atmosphere that is more dynamic than expected.
- Emmanuel Marcq
- , Jean-Loup Bertaux
- & Denis Belyaev
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News & Views |
Lunar water from the solar wind
The surface of the Moon is not totally devoid of water. Analyses of lunar soils reveal that impact glasses contain significant amounts of water, with an isotopic composition that is indicative of an origin from the solar wind.
- Marc Chaussidon
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Letter |
Direct measurement of hydroxyl in the lunar regolith and the origin of lunar surface water
Over the past few years, it has become clear that the Moon’s surface is not entirely dry. The direct identification of hydroxyl in glasses produced in lunar soils by the impact of micrometeorites supports the idea that water was delivered to the lunar surface by the solar wind.
- Yang Liu
- , Yunbin Guan
- & Lawrence A. Taylor
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News & Views |
Slippery sliding on icy Iapetus
Enigmatically, some landslides flow farther than normal frictional resistance allows. Cassini images of Saturn's icy moon Iapetus reveal a multitude of long-runout landslides that may have been enabled by flash heating along the sliding surface.
- Antoine Lucas
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Article |
Massive ice avalanches on Iapetus mobilized by friction reduction during flash heating
The great distance travelled by long-runout landslides, observed previously on the Earth and Mars, requires a mechanism of friction reduction. Identification and analysis of long-runout landslides on Saturn’s moon Iapetus suggests that the Iapetian landslides are enabled by flash heating of the icy sliding surface.
- Kelsi N. Singer
- , William B. McKinnon
- & Jeffery M. Moore
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Letter |
Late accretion as a natural consequence of planetary growth
The mantles of the terrestrial planets contain elemental abundances that suggest accretion continued at a late stage, after core formation. Geochemical data of meteorites from differentiated asteroids are consistent with such a late accretion event, suggesting that the phenomenon occurred throughout the Solar System and was related to planet formation.
- James M. D. Day
- , Richard J. Walker
- & Douglas Rumble III
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Editorial |
Sandblasted by the Sun
The Earth's magnetic field protects us from solar activity, but the Moon and Mars are more exposed. The upcoming solar maximum is the perfect time to observe how our dynamic Sun affects its planets.
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Letter |
Recent extensional tectonics on the Moon revealed by the Lunar Reconnaissance Orbiter Camera
On the Moon, extensional tectonic features have only been observed close to the influence of the mare basalt-filled basins and floor-fractured craters. Analysis of Lunar Reconnaissance Orbiter Camera images reveals several potentially very young extensional tectonic features in the farside highlands, implying that extensional stresses may locally exceed compressional ones.
- Thomas R. Watters
- , Mark S. Robinson
- & Brett W. Denevi
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Letter |
Two boundary layers in Titan’s lower troposphere inferred from a climate model
Saturn’s moon Titan has a dense atmosphere, but its thermal structure is poorly understood. Simulations with a three-dimensional general circulation model suggest that Titan has a lower atmospheric structure with two boundary layers: a seasonal deep layer, and a shallower one that develops during the course of each day.
- Benjamin Charnay
- & Sébastien Lebonnois
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Letter |
Equatorial winds on Saturn and the stratospheric oscillation
The stability over time of the zonal jets on the giant planets has been debated. An analysis of observations from the Cassini spacecraft reveals an acceleration of wind velocities in Saturn’s high-altitude equatorial jet between 2004 and 2009, by 20 m s−1 at tropopause level and by 60 m s−1 in the stratosphere.
- Liming Li
- , Xun Jiang
- & Kevin H. Baines
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News & Views |
Water on the Moon
Analysis of the first Apollo samples suggested that Earth's only satellite was bone dry. Spacecraft data and improved analysis techniques now indicate that the Moon is more volatile-rich and complex than previously thought.
- David J. Lawrence
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Letter |
Cold glacial oceans would have inhibited phyllosilicate sedimentation on early Mars
Phyllosilicate minerals are rare in the Noachian-aged crust of the northern lowlands of Mars, compared with the tropical highlands. Geochemical and climate modelling suggest that this dichotomy is consistent with the presence of a cold ocean fringed by cold-based glaciers.
- Alberto G. Fairén
- , Alfonso F. Davila
- & James F. Kasting
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News & Views |
Arrow in Titan's sky
An exotic arrow-shaped cloud was discovered in the atmosphere of Saturn's moon Titan last year. Numerical modelling shows how a large-scale atmospheric wave can naturally shape tropical clouds to such an arrow.
- Tetsuya Tokano
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Letter |
Locally enhanced precipitation organized by planetary-scale waves on Titan
Saturn’s moon Titan exhibits an active weather cycle that involves methane. An analysis of cloud observations and simulations with a general circulation model reveals that convection in Titan’s atmosphere is organized through an interplay of two wave modes, leading to local rates of precipitation of up to twenty times the average.
- Jonathan L. Mitchell
- , Máté Ádámkovics
- & Elizabeth P. Turtle
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News & Views |
More surprises from the Moon
Volcanic deposits on the Moon are almost entirely composed of basaltic lava flows that make up the dark and extensive mare plains. High-resolution images and compositional data now reveal rare, non-mare volcanism on the Moon's farside.
- Noah Petro
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Article |
Non-mare silicic volcanism on the lunar farside at Compton–Belkovich
Non-basaltic volcanism is rare on the Moon and has been found predominantly on the lunar nearside. Analysis of Lunar Reconnaissance Orbiter Camera images and spectral data reveal the presence of compositionally evolved, non-basaltic volcanism on the lunar farside.
- Bradley L. Jolliff
- , Sandra A. Wiseman
- & David A. Paige
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Letter |
Replacement and late formation of atmospheric N2 on undifferentiated Titan by impacts
The origin of Titan’s massive nitrogen atmosphere is largely unknown. Laser-gun experiments and numerical calculations suggest that the nitrogen could have been generated by conversion from ammonia during the period of Late Heavy Bombardment.
- Yasuhito Sekine
- , Hidenori Genda
- & Takafumi Matsui
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News & Views |
Gathering dust
Chondritic meteorites are remnants of the ancient Solar System. Analysis of the dust rims often found on their constituent particles shows that the rims were swept up while the particles wafted about and collided in a weakly turbulent protoplanetary nebula.
- Jeff Cuzzi