Nature Geoscience
Nature Geoscience, Published online: 08 September 2026; doi:10.1038/s41561-026-02085-z The soot fraction of global black carbon emissions increased from 16% in 1750 to 35% in 2019, mainly driven by fossil fuel consumption, suggesting a higher warming potential per unit mass, according to an analysis of atmospheric measurements.
Nature Geoscience, Published online: 08 September 2026; doi:10.1038/s41561-026-02088-w The minerals needed to transport water into the deepest parts of the Earth’s mantle remain unclear. High-pressure and -temperature experiments conducted at lower-mantle conditions suggest that iron oxyhydroxide phases may be important to such transport.
Nature Geoscience, Published online: 08 September 2026; doi:10.1038/s41561-026-02067-1 Dense iron oxyhydroxide phases may form from an early basal magma ocean, trapping water and potentially contributing to the formation of thermochemical anomalies in the deep mantle, according to high-pressure and high-temperature experiments.
Nature Geoscience, Published online: 07 September 2026; doi:10.1038/s41561-026-02086-y During the last ice age, the Atlantic Meridional Overturning Circulation (AMOC) underwent a series of abrupt reorganizations. The global impact of these events reflects the accumulation of heat in the ocean interior during the weak AMOC mode and its loss during the strong mode, facilitated by radiative feedback…
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02084-0 Biocrusts can substantially enhance snow retention, sustaining soil biogeochemistry, microbial activity and soil ecosystem functions in cold deserts, according to a long-term field study of how moss-dominated biocrust cover influences snow cover duration and depth.
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02079-x Nature-based solutions in savannas and grasslands that seek to maximize tree cover and carbon uptake can erode biodiversity, create fragile carbon stocks and disrupt the livelihoods of people who depend on these landscapes, all for uncertain climate benefits.
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02087-x Nature Geoscience spoke with Ana Bastos (Leipzig University, Germany) and Sonia I. Seneviratne (ETH Zürich, Switzerland) about how climate change is reshaping forest ecosystems, how forests and land-use change feedback on the climate system, and what this means for land-based climate mitigation strategies.
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02105-y Advances in forest monitoring techniques are transforming our understanding of how forests gain and lose carbon, respond to environmental change, and influence climate. These insights highlight the potential and limitations of forest-based climate solutions.
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02066-2 The build-up of soil organic carbon depends less on the amount of substrate carbon available but more on the energy soil microbes can use to grow and leave behind residues, according to a global analysis of microbial energy demand and the energy contained in substrate carbon.
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02081-3 Satellites are revolutionizing our ability to observe forest ecosystems from space, especially when integrated with field observations, experiments and models. The greatest challenge is no longer a lack of observations, but rather the integration of information and knowledge across scales to better understand r…
Nature Geoscience, Published online: 04 September 2026; doi:10.1038/s41561-026-02065-3 Siderite has a debated formation route — abiotic or microbially mediated — with implications for both the early Earth and Mars, as Neha Mehta explains.
Nature Geoscience, Published online: 03 September 2026; doi:10.1038/s41561-026-02095-x Drought disturbances are reducing the recovery capacity of tropical forests, especially in drier conditions, but soil phosphorus can mitigate this impact, according to a satellite-based analysis of ecosystem resilience.
Nature Geoscience, Published online: 01 September 2026; doi:10.1038/s41561-026-02083-1 Vertically compound soil moisture droughts—when all soil layers are depleted—have intensified worldwide, driving sharper ecosystem losses than single-layer droughts, according to global analyses of multilayer soil moisture.
Nature Geoscience, Published online: 31 August 2026; doi:10.1038/s41561-026-02090-2 Single-cell Hadley circulation drives pole-to-pole connection on Mars but also inhibits material mixing between the cell’s interior and exterior, according to a study of the Martian atmosphere using Lagrangian particle tracking.
Nature Geoscience, Published online: 27 August 2026; doi:10.1038/s41561-026-02108-9 Author Correction: Antarctic greening is constrained by biology and requires field validation
Nature Geoscience, Published online: 25 August 2026; doi:10.1038/s41561-026-02071-5 Forest disturbances drive substantial surface warming across Europe, with magnitude and recovery shaped by disturbance severity, size and forest characteristics, as inferred from combining satellite-derived land-surface temperature estimates with continent-wide disturbance data.
Nature Geoscience, Published online: 25 August 2026; doi:10.1038/s41561-026-02068-0 Layers of particulate matter that accumulate on black carbon can boost warming by raising top-of-atmosphere forcing, with biomass-burning particles two to three times more impactful than urban ones, based on a model and global observations.
Nature Geoscience, Published online: 25 August 2026; doi:10.1038/s41561-026-02092-0 Coatings on black carbon particles modulate their warming potential. A decade of global single-particle observations shows that the amount of coating scales with the ratio of particulate matter smaller than 2.5 μm in diameter to black carbon mass, enabling the warming effect of black carbon to be evaluated worldwi…
Nature Geoscience, Published online: 21 August 2026; doi:10.1038/s41561-026-02078-y Uncertain internal variability in Arctic warming
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