Mike Weber, ” Sediments Offer an Extended History of Fast Ice”
EARTH SCIENCE ARCHIVE
Oysters Clean Up More Nitrogen Pollution Than We Thought
New research has revealed that significant amounts of excess nitrogen in coastal waters are buried as oyster reefs grow and that some reefs trap more nitrogen than others.
6.16亿年前波罗的大陆在哪里？
通过解析古老岩石中的磁信号，我们得以重新认识这块古大陆在埃迪卡拉纪时期的位置。
A Unique African Volcano Could Solve a Mystery on Mercury
New data from Ol Doinyo Lengai in Tanzania suggest that carbon-rich volcanic activity could be responsible for the mysterious “hollows” observed on the surface of Mercury.
Pre-Existing Structure and Stress Shape Geothermal-Induced Seismicity
At China’s first Enhanced Geothermal System site, dense seismic observations, integrated with borehole data and stress modeling, reveal weak faults and scale-dependent control of stress and structure on induced seismicity.
Model of Complex Blanket Bog Improves Prediction of Peat Expansion
Peat expansion is tightly coupled to the global climate cycle. As a nature-based solution to climate change, we need to know how they will respond to different climate scenarios.
An Off-Road Itinerary
This month, we cover the work of scientists stepping out of their labs and into the field, from rugged lava expanses and volcanic summits to arid ice sheets and lake beds.
Ancient Subduction May Have Seeded Today’s Critical Mineral Deposits
The fertilized mantle lithosphere may play an important first step in the formation of carbonatite deposits, known to host critical minerals.
Repairing the Ozone Layer May Take Longer Than Expected
A new study reveals that if left unchecked, unaccounted-for emissions of ozone-harming substances could delay the layer’s full recovery by almost a decade.
The Governance Gap Threatening Long-Term Ecological Archives
To save multigenerational science from administrative indifference, we must mandate stewardship continuity before closing physical facilities.
Heavy Rainfall Inflates Mount Fuji
The uplift, several centimeters in magnitude, is likely caused by water pooling in the mountain’s shallow aquifers. The effect is shorter lived than deformation caused by magmatic activity.
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