Results 191 to 200 of about 50,990 (290)
Magmatic domes and the initiation of oceanic processes at the Norwegian margin. [PDF]
Peron-Pinvidic G.
europepmc +1 more source
Abstract The subtropical North Atlantic is a key region for ocean carbon cycling despite its relatively small spatial extent. Here we present a high‐resolution transect (23°–27°N; ∼2° longitude spacing) across the North Atlantic Subtropical Gyre, integrating physical, chemical, and microbial observations to examine how hydrography and nutrient ...
Lukas Marx +5 more
wiley +1 more source
Linking electrical anomalies in the upper mantle to petrological and geochemical heterogeneities. [PDF]
Yang X, Xu YG, Xia QK.
europepmc +1 more source
A Sea‐Ice‐Enhanced KPP Parameterization: Impacts on AMOC Simulation and Physical Pathways
Abstract This study presents a sea‐ice‐enhanced K‐profile parameterization to improve simulations of the Atlantic Meridional Overturning Circulation (AMOC) in ocean–sea ice coupled models. The modified KPP dynamically scales the background vertical diffusivity with local sea‐ice fraction, representing the insulating and turbulence‐suppressing effects ...
Yu‐Heng Tseng, Yi‐Wen Wang
wiley +1 more source
Environmental Adaptation Strategies of Deep-Sea Fungi. [PDF]
Leng S, Liu CH.
europepmc +1 more source
Thermal Segregation and Reddening in Europa's Double Ridges
Abstract Europa's double ridges often display lower albedo and redder color than their surroundings. Their unique topography may cause sublimation‐driven darkening due to illumination and self‐heating—the process of thermal segregation. We apply an advanced 3D thermophysical model, including shadowing and self‐heating through mutual exchange of ...
Kya C. Sorli +3 more
wiley +1 more source
Oceanic upper crustal accretion by melt sill and lava flow interaction at Axial volcano. [PDF]
Wu H +6 more
europepmc +1 more source
Abstract Proxy records of seawater radiocarbon (14C/C) provide strong constraints on how changes in ocean ventilation contributed to the increase in atmospheric CO2 during the termination of the last ice age (≈18,000‐to‐12,000 years ago). One outstanding problem, however, is the existence of anomalously low deglacial benthic foraminiferal 14C/C in the ...
Patrick A. Rafter +14 more
wiley +1 more source
Enigmatic carbon isotopic variability in the oceanic upper mantle. [PDF]
Moussallam Y +9 more
europepmc +1 more source

