Mantle Dynamic Topography of the Fringing Oceanic Basins of Antarctica
Abstract Dynamic mantle processes are known to influence oceanic basins with implications for ocean circulation and climate. This study exploits an interdisciplinary approach to probe present‐day mantle and lithosphere beneath Antarctica's fringing oceanic basins to better understand sub‐crustal processes and implications for the continental realm.
A. C. A. Dunn +4 more
wiley +1 more source
Anomalous K-Pg-aged seafloor attributed to impact-induced mid-ocean ridge magmatism. [PDF]
Byrnes JS, Karlstrom L.
europepmc +1 more source
Climate Change Impacts on Hydrology in the Upper James Watershed, Virginia
ABSTRACT Hydrological modeling of the Upper James Watershed (UJW), Virginia, is critical for predicting water availability, flood management, agriculture, ecosystem protection, and hydropower production under increasing climate change. The Hydrologic Engineering Center–Hydrologic Modeling System (HEC‐HMS) is applied to evaluate climate change impacts ...
Imiya Mudiyanselage Chathuranika +1 more
wiley +1 more source
Correction for Worman et al., Abiotic hydrogen (H2) sources and sinks near the Mid-Ocean Ridge (MOR) with implications for the subseafloor biosphere. [PDF]
europepmc +1 more source
Discovery of a Thermostable GH10 Xylanase with Broad Substrate Specificity from the Arctic Mid-Ocean Ridge Vent System. [PDF]
Fredriksen L +6 more
europepmc +1 more source
ABSTRACT Mesophotic reefs are located in low light conditions which, depending on the region, are usually found in water depths greater than ~30 m. They are less affected by ocean warming than reefs found in shallower water depths and thus might become increasingly important for the sustainability of marine biodiversity.
Or M. Bialik +7 more
wiley +1 more source
Seafloor hydrothermal activity along mid-ocean ridge with strong melt supply: study from segment 27, southwest Indian ridge. [PDF]
Yue X +6 more
europepmc +1 more source
ABSTRACT The Gollum Channel System is a land‐detached large‐scale canyon‐channel system situated offshore southwest Ireland on the Northeast Atlantic margin. The system has been considered inactive with downslope gravity flows since the last glacial period, but geophysical data in some of its branches do suggest Holocene activity.
Lotte Verweirder +8 more
wiley +1 more source
Large melt diversity at a mid-ocean ridge thermal low. [PDF]
Brunelli D +8 more
europepmc +1 more source
Magma plumbing system and seismicity of an active mid-ocean ridge volcano. [PDF]
Schmid F +4 more
europepmc +1 more source

