Results 131 to 140 of about 20,448 (261)
Abstract Degradation of Arctic permafrost due to global warming and sea level rise could trigger positive feedbacks, exacerbating climate change. However, uncertainties remain on how permafrost systems may respond because we lack a complete understanding of the permafrost‐climate feedback.
Mathia Sabino +6 more
wiley +1 more source
The Contested Adriatic Sea: The Adriatic Guard and Identity Politics in Interwar Yugoslavia
Throughout history, Mediterranean cultures have tried to appropriate, with words or weapons, the sea that surrounds them. Sometimes called the “Inner Sea,” “Superior Sea,” or “Great Sea,” the Mediterranean was designated by the Greeks—as the Odyssey ...
Igor Tchoukarine
core +1 more source
Arc Heat Flow and Magmatic Heat Budgets
Abstract We evaluate hydrothermal heat loss from 11 volcanic‐arc segments (∼6,000 km of arc length, ∼10% of the global total), motivated by the observation that much magmatic heat ultimately crosses the land surface as heated aqueous fluid. Heat loss takes place by volcanic eruption, geothermal heat conduction to the surface, fumarolic (vapor ...
S. E. Ingebritsen +7 more
wiley +1 more source
Relief shown by hachures and spot heights. Depths shown by contours and soundings.; Base map: Mediterranean Sea, Adriatic Sea : 12th ed., May 1938, no. 3919 / U.S. Navy, Hydrographic Office.; "Annex no.
core
Abstract Marine carbonate carbon isotopes (δ13C), over orbital to multi‐million‐year timescales, provide critical insight into the carbon cycle connecting Earth's atmosphere, lithosphere, hydrosphere and biosphere. However, the influence of astronomical forcing on deep time carbon cycle dynamics remains poorly constrained.
Deyan Zhang +4 more
wiley +1 more source
Long‐Term Deformation in the Alpine‐Provence Foreland Constrained by In Situ Calcite U‐Pb Dating
Abstract The evolution of the Alpine‐Provence foreland is characterized by multiple deformation phases since the Mesozoic, representing successive compressional and extensional episodes. The precise timing and spatial evolution of these deformation phases remain poorly constrained due to the lack of absolute geochronological data. Here, we present U–Pb
Dorian Bienveignant +12 more
wiley +1 more source
Changes in DOM composition influence prokaryotic species growth in the Mediterranean Sea, shaping their metabolic responses and organic matter processing. In our study, higher DOP consumption and alkaline phosphatase activity led to the accumulation of recalcitrant DOM, highlighting how microbial community shifts drive distinct pathways in carbon ...
Eva Ortega‐Retuerta +9 more
wiley +1 more source
ABSTRACT Since 2000, archaeological excavations have brought to light the sanctuary of Athena in Castro (Apulia, Italy), including terracotta roofs dated between the 6th and 4th centuries bce. Based on their morphological and stylistic features, it is suggested that the terracotta items were manufactured in the Greek colony of Taras (modern Taranto ...
M. M. N. Franceschini +7 more
wiley +1 more source
Paradox of Value Loops in Dynamic Markets: From Value Post‐(Un)capture to Sustainable Recapture
ABSTRACT The growing emphasis on sustainability necessitates a re‐evaluation of traditional value creation and capture challenges, highlighting the intricate interrelation between value (un)captured and recaptured. This study investigates the dynamics of overtourism and undertourism in the sustainable development of regions. This prominent incidence of
Agnieszka Kabalska +2 more
wiley +1 more source
ABSTRACT Aim This research investigates the distribution of the non‐indigenous calanoid copepod Pseudodiaptomus marinus Sato, 1913 in Italian coastal waters as retrieved by the data collected in the Marine Strategy Framework Directive (MSFD) programme in the 2015–2023 time window. Location Italian marine coastal waters, Mediterranean Sea.
Stefano Corona +7 more
wiley +1 more source

