Results 51 to 60 of about 25,230 (195)
δ18O of atmospheric oxygen measured on the GRIP Ice Core Document Stratigraphic disturbances in the lowest 10% of the core [PDF]
δ18O measured on oxygen in the bubble air from ice cores is a proxy for continental ice volume and is used to synchronize cores from Greenland and Antarctica.
Fuchs, Andreas, Leuenberger, Markus C.
core +1 more source
ABSTRACT The timing and spatial patterns of glaciers retreat in the Northern French Alps during the Lateglacial (19.0–11.7 ka) remain debated, reflecting discrepancies among available chronological data sets. The complex interactions between major glaciers, such as the Rhône and Arve glaciers to the north and the Isère glacier to the south, represent a
Quentin Portal +3 more
wiley +1 more source
Data-model comparison of soil–water δ18O at a temperate site in N. Spain with implications for interpreting speleothem δ18O [PDF]
An understanding of how seasonal and longer-term δ18O signals in meteoric precipitation (δ18Op) are modified by percolation through soils is essential to link temporal changes in speleothem δ18O to surface climatic conditions.
McDermott, Frank, Comas-Bru, Laia
core +1 more source
Tracing fluid transfers in subduction zones: an integrated thermodynamic and δ18O fractionation modelling approach [PDF]
Oxygen isotope geochemistry is a powerful tool for investigating rocks that interacted with fluids, to assess fluid sources and quantify the conditions of fluid–rock interaction. We present an integrated modelling approach and the computer program PTLoop
Vho, Alice +3 more
core +2 more sources
ABSTRACT Enamel hypoplasia results from temporary disruptions of enamel deposition during tooth development. It is widely used as an indicator of physiological stress in archeological and paleontological contexts; yet, its relationship with environmental conditions during tooth formation remains poorly constrained.
Giuseppe Briatico +3 more
wiley +1 more source
Abstract Worldwide, lacustrine ecosystems are threatened by eutrophication and deoxygenation. Both processes are driven by the combined effects of human activities and climate change. Understanding the pre‐anthropogenic nexus between warming, eutrophication, deoxygenation, and related feedback is essential to determine how lakes respond to rapid ...
Noé R.M.M. Schmidhauser +7 more
wiley +1 more source
South Atlantic Multi‐Site Calibration of Coral Oxygen Isotope Paleothermometer
Coral‐based stable oxygen isotopes (δ18O) have been used as a proxy for sea surface temperature (SST) since the 1970s, and δ18O–SST calibration studies have been fundamental to assure robust and faithful SST reconstructions.
N. S. Pereira +10 more
doaj +1 more source
Fish without water: Validation and application of δ18O in Totoaba macdonaldi otoliths
The geochemistry of fish otoliths is a valuable tool for reconstructing environmental conditions, migrations and life histories. In this study we validate the relationship between temperature, the water oxygen isotope composition (δ18O) and otolith δ18O
K Rowell, C True, KW Flessa, DL Dettman
doaj +1 more source
Calcite cement is a common diagenetic mineral in carbonate rocks and plays an important role on rock quality as hydrocarbon reservoirs. Traditionally, oxygen isotopic compositions (δ18O) of the diagenetic calcites tend to decrease with increasing depths ...
Guangwei Wang +5 more
doaj +1 more source
ABSTRACT Deep‐rooted plantations are central to dryland ecological restoration, yet their long‐term cultivation drives widespread deep soil desiccation, threatening ecosystem sustainability. While artificial water replenishment is a key deep soil desiccation mitigation strategy, the depth‐dependent positional effect of stored water on eco‐hydrological ...
Haoyan Wei +6 more
wiley +1 more source

