Home > Search Results: Bostock, Helen
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Articles, 2 records found
Articles 2 records found  
1.
19 p, 3.7 MB Reduction in size of the calcifying phytoplankton Calcidiscus leptoporus to environmental changes between the Holocene and modern Subantarctic Southern Ocean / Rigual-Hernández, Andrés S. (Universidad de Salamanca. Departamento de Geología) ; Langer, Gerald (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals) ; Sierro, Francisco Javier (Universidad de Salamanca. Departamento de Geología) ; Bostock, Helen (University of Queensland) ; Sánchez-Santos, José Manuel (Universidad de Salamanca. Departamento de Estadística) ; Nodder, Scott Davidson (National Institute of Water and Atmospheric Research) ; Trull, Tom W. (Commonwealth Scientific and Industrial Research Organisation) ; Ballegeer, Anne Marie (Universidad de Salamanca. Departamento de Didáctica de las Matemáticas y de las Ciencias Experimentales) ; Moy, Andrew D. (University of Tasmania) ; Eriksen, Ruth (Commonwealth Scientific and Industrial Research Organisation) ; Makowka, Laura (Universidad de Salamanca. Departamento de Geología) ; Béjard, Thibauld M. (Universidad de Salamanca. Departamento de Geología) ; Rigal-Muñoz, Francisco Henri (Universidad de Salamanca. Departamento de Geología) ; Hernández-Martín, Alberto (Universidad de Salamanca. Departamento de Geología) ; Zorita-Viota, María (Universidad de Salamanca. Departamento de Geología) ; Flores, José Abel (Universidad de Salamanca. Departamento de Geología)
The Subantarctic Zone of the Southern Ocean plays a disproportionally large role on the Earth system. Model projections predict rapid environmental change in the coming decades, including ocean acidification, warming, and changes in nutrient supply which pose a serious risk for marine ecosystems. [...]
2023 - 10.3389/fmars.2023.1159884
Frontiers in marine science, Vol. 10 (June 2023) , art. 1159884  
Detailed record - Creative Commons
2.
19 p, 6.1 MB Calibration of the carbon isotope composition (δ13C) of benthic foraminifera / Schmittner, Andreas (Oregon State University. College of Earth, Ocean and Atmospheric Sciences) ; Bostock, Helen (National Institute of Water and Atmospheric Research) ; Cartapanis, Olivier (University of Bern. Institute of Geological Sciences and Oeschger Center for Climate Change Research) ; Curry, William B. (Bermuda Institute of Ocean Sciences) ; Filipsson, Helena L. (Lund University. Department of Geology) ; Galbraith, Eric (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals) ; Gottschalk, Julia (University of Bern. Institute of Geological Sciences and Oeschger Center for Climate Change Research) ; Herguera, Juan Carlos (Centro de Investigación Científica y Educación Superior de Ensenada. México.) ; Hoogakker, Babette (Heriot Watt University. Edinburgh) ; Jaccard, Samuel L. (University of Bern. Institute of Geological Sciences and Oeschger Center for Climate Change Research) ; Lisiecki, Lorraine (University of California. Department of Earth Sciences) ; Lund, David C. (University of Connecticut-Avery Point. Department of Marine Sciences) ; Martínez Méndez, Gema (University of Bremen. MARUM-Center for Marine Environmental Sciences) ; Lynch-Stieglitz, Jean (Georgia Institute of Technology. School of Earth and Atmospheric Sciences) ; Mackensen, Andreas (Alfred-Wegener-Institut für Polar- und Meeresforschung) ; Michel, Elisabeth (Laboratoire des sciences du climat et de l'environnement (LSCE)) ; Mix, Alan C. (Oregon State University. College of Earth, Ocean and Atmospheric Sciences) ; Oppo, Delia W. (Woods Hole Oceanographic Institution) ; Peterson, Carlye D. (University of California. Department of Earth and Planetary Sciences) ; Repschläger, Janne (Max Planck Institute for Chemistry. Germany) ; Sikes, Elisabeth L. (Rutgers University. Institute of Marine and Coastal Sciences) ; Spero, Howard J. (University of California. Department of Earth and Planetary Sciences) ; Waelbroeck, Claire (Laboratoire des sciences du climat et de l'environnement (LSCE))
The carbon isotope composition (δ13C) of seawater provides valuable insight on ocean circulation, air-sea exchange, the biological pump, and the global carbon cycle and is reflected by the δ13C of foraminifera tests. [...]
2017 - 10.1002/2016PA003072
Paleoceanography, Vol. 32, issue 6 (June 2017) , p. 512-530  
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