4.7 Article

Constraining the marine strontium budget with natural strontium isotope fractionations (87Sr/86Sr*, δ88/86Sr) of carbonates, hydrothermal solutions and river waters

Journal

GEOCHIMICA ET COSMOCHIMICA ACTA
Volume 74, Issue 14, Pages 4097-4109

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2010.04.009

Keywords

-

Funding

  1. Deutsche Forschungsgemeinschaft, DFG [Ei272/29-1, Ei272/30-1]

Ask authors/readers for more resources

We present strontium (Sr) isotope ratios that, unlike traditional Sr-87/Sr-86 data, are not normalized to a fixed Sr-88/Sr-86 ratio of 8.375209 (defined as delta Sr-88/86 = 0 relative to NIST SRM 987). Instead, we correct for isotope fractionation during mass spectrometry with a Sr-87-Sr-84 double spike. This technique yields two independent ratios for Sr-87/Sr-86 and Sr-88/Sr-86 that are reported as (Sr-87/Sr-86*) and (delta Sr-88/86), respectively. The difference between the traditional radiogenic (Sr-87/Sr-86 normalized to Sr-88/Sr-86 = 8.375209) and the new Sr-87/Sr-86* values reflect natural mass-dependent isotope fractionation. In order to constrain glacial/interglacial changes in the marine Sr budget we compare the isotope composition of modern seawater ((Sr-87/Sr-86*, delta Sr-88/86)(Seawater)) and modern marine biogenic carbonates ((Sr-87/Sr-86*, delta(88)/Sr-86)(Carbonates)) with the corresponding values of river waters ((Sr-87/Sr-86*, delta Sr-88/86)(River)) and hydrothermal solutions ((Sr-87/Sr-86*, delta(88)/Sr-86)(HydEnd)) in a triple isotope plot. The measured (Sr-87/Sr-86*, delta(88)/Sr-86)(River)). values of selected rivers that together account for similar to 18% of the global Sr discharge yield a Sr flux-weighted mean of (0.7114(8), 0.315(8)parts per thousand). The average ((Sr-87/Sr-86*, delta Sr-88/86)(HydEnd) values for hydrothermal solutions from the Atlantic Ocean are (0.7045(5), 0.27(3)parts per thousand). In contrast, the (Sr-87/Sr-86*, delta Sr-88/86)(Carbonates) values representing the marine Sr output are (0.70926(2), 0.21(2)parts per thousand). We estimate the modern Sr isotope composition of the sources at (0.7106(8), 0.310(8)parts per thousand). The difference between the estimated (Sr-87/Sr-86*, delta Sr-88/86) and (Sr-87/Sr-86*, delta(88)/Sr-86)(output) values reflects isotope disequilibrium with respect to Sr inputs and outputs. In contrast to the modern ocean, isotope equilibrium between inputs and outputs during the last glacial maximum (10-30 ka before present) can be explained by invoking three times higher Sr inputs from a uniquely glacial source: weathering of shelf carbonates exposed at low sea levels. Our data are also consistent with the weathering peak hypothesis that invokes enhanced Sr inputs resulting from weathering of postglacial exposure of abundant fine-grained material. (C) 2010 Elsevier Ltd. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Biology

Coccolith volume of the Southern Ocean coccolithophoreEmiliania huxleyias a possible indicator for palaeo-cell volume

Marius N. Mueller, Frederico P. Brandini, Thomas W. Trull, Gustaaf M. Hallegraeff

Summary: The study found that environmental factors such as temperature, irradiance, carbonate chemistry, and macronutrient limitation significantly affect the coccosphere, coccolith, and cell volume of the Southern Ocean Emiliania huxleyi ecotype A. There is a strong correlation between cell and coccolith volume, indicating that coccolith volume is primarily controlled by physiological changes in cell volume. Macronutrient limitation, particularly of phosphorus and nitrogen, has the greatest influence on coccolith volume compared to other environmental drivers.

GEOBIOLOGY (2021)

Article Multidisciplinary Sciences

13 million years of seafloor spreading throughout the Red Sea Basin

Nico Augustin, Froukje M. van der Zwan, Colin W. Devey, Bryndis Brandsdottir

Summary: Based on earthquake data, vertical gravity gradient data and high-resolution bathymetry, the research indicates that the Red Sea is a mature ocean basin where continuous seafloor spreading began along its entire length around 13 million years ago.

NATURE COMMUNICATIONS (2021)

Article Geochemistry & Geophysics

Microseismicity and Lava Flows Hint at Magmato-Tectonic Processes Near the Southern Tip of the Fonualei Rift and Spreading Center in the Lau Basin

F. Schmid, M. Cremanns, N. Augustin, D. Lange, F. Petersen, H. Kopp

Summary: The researchers located 697 micro-earthquakes at the southern Fonualei Rift and Spreading Center and found that most epicenters concentrated along the central region of the axial valley, with a majority of events associated with a 138-hour lasting earthquake swarm. The tectonic structure of the ridge axis in the S-FRSC resembles a series of left-stepping en echelon segments expressed at the seafloor by numerous volcanic ridges.

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH (2021)

Article Multidisciplinary Sciences

Survival of presolar p-nuclide carriers in the nebula revealed by stepwise leaching of Allende refractory inclusions

Bruce L. A. Charlier, Francois L. H. Tissot, Hauke Vollstaedt, Nicolas Dauphas, Colin J. N. Wilson, Ren T. Marquez

Summary: Experimental results on CAIs from the Allende meteorite suggest that extreme Sr-84 anomalies may be caused by the presence of a presolar carrier enriched in the p-nuclide Sr-84. This discovery reinstates the chronological significance of differences in initial Sr-87/Sr-86 ratios between CAIs and volatile-depleted inner solar system materials.

SCIENCE ADVANCES (2021)

Article Environmental Sciences

Biogeochemical feedbacks may amplify ongoing and future ocean deoxygenation: a case study from the Peruvian oxygen minimum zone

Klaus Wallmann, Yonss S. Jose, Mark J. Hopwood, Christopher J. Somes, Andrew W. Dale, Florian Scholz, Eric P. Achterberg, Andreas Oschlies

Summary: A new model is used to simulate the nutrient cycling in the Peruvian oxygen minimum zone. The model shows that dissolved iron is the limiting nutrient for primary production and is released from sediments. Simulations indicate that the productivity of the OMZ will increase due to enhanced iron release. However, further phytoplankton growth will be limited by the loss of reactive nitrogen.

BIOGEOCHEMISTRY (2022)

Article Geochemistry & Geophysics

New Perspectives on the 143Nd/144Nd Palaeoceanographic Tracer on Foraminifera: The State-of-the-Art Frontiers of Analytical Methods

Filip Scheiner, Lukas Ackerman, Katarina Holcova, Jan Rejsek, Hauke Vollstaedt, Jana Durisova, Vaclav Santolik

Summary: The Nd-143/Nd-144 isotopic composition of foraminifera is a useful proxy for tracing specific water masses in paleoceanographic studies, but its applicability is limited by the amount of material needed for analysis. In this study, we analyzed foraminiferal samples weighing only 300-500 μg and showed that even very low Nd loads can yield precise results. We also found significant naturally induced Nd isotopic variability among different foraminiferal species.

GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS (2022)

Article Limnology

Thermal plasticity of coral reef symbionts is linked to major alterations in their lipidome composition

Marina T. Botana, Adriano B. Chaves-Filho, Alex Inague, Arthur Z. Guth, Flavia Saldanha-Correa, Marius N. Muller, Paulo Y. G. Sumida, Sayuri Miyamoto, Matthias Y. Kellermann, Raymond C. Valentine, Marcos Y. Yoshinaga

Summary: Coral decline caused by ocean warming is a global issue. This study used an untargeted lipidomic approach to examine the changes in lipidome and pigments of coral symbionts after a heat shock. The results showed that heat sensitive symbionts displayed changes in lipidome and pigments, while heat tolerant symbionts maintained stable membrane lipids. These findings provide a baseline for further research on lipid biomarkers linked to thermal stress.

LIMNOLOGY AND OCEANOGRAPHY (2022)

Article Geochemistry & Geophysics

Early stage diapirism in the Red Sea deep-water evaporites: Origins and length-scales

Neil C. Mitchell, Karina Hernandez, Jonas Preine, Marco Ligi, Nico Augustin, Ay Izzeldin, Christian Huebscher

Summary: Rayleigh-Taylor models predict that diapirs should develop with characteristic spacings, but our study on the deep-water Miocene evaporites in the Red Sea shows that the diapirism does not have a uniform scale. The topography of the S-reflection indicates stochastic behavior with a range of around 3 km. The Rayleigh-Taylor model does not explain the deformation in the Red Sea evaporites. The findings provide insights into the vertical and length scales of early-stage salt giants.

TECTONOPHYSICS (2022)

Editorial Material Environmental Sciences

Editorial: Sustainable Development Goal 14-Life Below Water: Towards a Sustainable Ocean

Brett W. W. Molony, Alex T. T. Ford, Ana M. M. Sequeira, Angel Borja, Anna Milena Zivian, Carol Robinson, Christian Lonborg, Elva G. G. Escobar-Briones, Emanuele Di Lorenzo, Jesper H. H. Andersen, Marius N. N. Mueller, Michelle J. J. Devlin, Pierre Failler, Sebastian Villasante, Simone Libralato, Tomaso Fortibuoni

FRONTIERS IN MARINE SCIENCE (2022)

Article Biotechnology & Applied Microbiology

Light induces peridinin and docosahexaenoic acid accumulation in the dinoflagellate Durusdinium glynnii

Carlos Yure B. Oliveira, Jessika L. Abreu, Elizabeth P. Santos, Angelo P. Matos, Giustino Tribuzi, Cicero Diogo L. Oliveira, Bruno O. Veras, Railson S. Bezerra, Marius N. Muller, Alfredo O. Galvez

Summary: This study investigated the effects of irradiance mediated by light-emitting diodes on growth performance, carotenoid and fatty acid profiles, and antioxidant activity of the endosymbiotic dinoflagellate Durusdinium glynnii. The results showed that D. glynnii is well adapted to low-light conditions but can also tolerate high light intensities. The accumulation of peridinin, a light-harvesting carotenoid, in D. glynnii occurred during high-light exposure. The study contributes to understanding the photoprotective role of peridinin in endosymbiont dinoflagellates and highlights the antioxidant activity of peridinin-rich extracts.

APPLIED MICROBIOLOGY AND BIOTECHNOLOGY (2022)

Article Biology

Palaeontological evidence for community-level decrease in mesopelagic fish size during Pleistocene climate warming in the eastern Mediterranean

Konstantina Agiadi, Frederic Quillevere, Rafal Nawrot, Theo Sommeville, Marta Coll, Efterpi Koskeridou, Jan Fietzke, Martin Zuschin

Summary: Mesopelagic fishes play crucial roles in marine food webs, are a vast but largely untapped food resource, and contribute significantly to the biological carbon pump. However, their future under climate change scenarios remains uncertain.

PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES (2023)

Article Geochemistry & Geophysics

Sources of Inaccuracy in Boron Isotope Measurement Using LA-MC-ICP-MS

Jan Fietzke, Eleni Anagnostou

Summary: Laser ablation multi-collector-inductively coupled plasma-mass spectrometry (LA-MC-ICP-MS) is a valuable tool for in situ measurement of boron isotope composition in geological samples, but it faces significant analytical challenges. This study focuses on the underlying processes causing inaccuracies in this technique, including the contribution of Ca and Ar ions to spectral baselines and the impact of plasma conditions on analytical biases. Experimental data and a release and diffusion model (RDM) suggest that a nearly complete release of boron from aerosol samples is necessary for consistently accurate measurement results without corrections.

GEOSTANDARDS AND GEOANALYTICAL RESEARCH (2023)

Article Environmental Sciences

New insights on the role of nitrogen in the resistance to environmental stress in an endosymbiotic dinoflagellate

Carlos Yure B. Oliveira, Barbara de Cassia S. Brandao, Luiz Gustavo de S. Jannuzzi, Deyvid Willame S. Oliveira, Gilvan Takeshi Yogui, Marius N. Mueller, Alfredo O. Galvez

Summary: This study explores how endosymbiotic dinoflagellates are affected by concentration and source of nitrogen. The results show that high nitrogen concentrations promote dinoflagellate growth, while the uptake of urea can alleviate the impact of thermal stress on the dinoflagellates, thus mitigating coral bleaching events.

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH (2023)

Article Multidisciplinary Sciences

Distinct fine-scale variations in calcification control revealed by high-resolution 2D boron laser images in the cold-water coral Lophelia pertusa

Jan Fietzke, Marlene Wall

Summary: Coral calcification is a complex process influenced by environmental conditions. The chemical composition of coral skeletons provides insights into the control exerted by the organism and the environment. This study found that there are differences in calcification control at different stages of skeleton formation in the cold-water coral Lophelia pertusa.

SCIENCE ADVANCES (2022)

Correction Multidisciplinary Sciences

Global variability in seawater Mg:Ca and Sr:Ca ratios in the modern ocean (vol 117, pg 22281, 2020)

Mario Lebrato, Dieter Garbe-Schonberg, Marius N. Muller, Sonia Blanco-Ameijeiras, Richard A. Feely, Laura Lorenzoni, Juan -Carlos Molinero, Karen Bremer, Daniel O. B. Jones, Debora Iglesias-Rodriguez, Dana Greeley, Miles D. Lamare, Aurelien Paulmier, Michelle Graco, Joan Cartes, Joana Barcelos e Ramos, Ana de Lara, Ricardo Sanchez-Leal, Paz Jimenez, Flavio E. Paparazzo, Susan E. Hartman, Ulrike Westernstroer, Marie Kuter, Roberto Benavides, Armindo F. da Silva, Steven Bell, Chris Payne, Solveig Olafsdottir, Kelly Robinson, Liisa M. Jantunen, Alexander Korablev, Richard J. Webster, Elizabeth M. Jones, Olivier Gilg, Pascal Bailly du Bois, Jacek Beldowski, Carin Ashjian, Nejib D. Yahia, Benjamin Twining, Xue-Gang Chen, Li-Chun Tseng, Jiang-Shiou Hwang, Hans-Uwe Dahms, Andreas Oschlies

Summary: The study found that seawater Sr:Ca values were systematically low due to normalization to IAPSO composition and the largest contribution to expanded uncertainty came from the uncertainty of the IAPSO reference composition. Additional factors should be considered to improve the accuracy of the data.

PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2021)

Article Geochemistry & Geophysics

Uranium isotopes in non-euxinic shale and carbonate reveal dynamic Katian marine redox conditions accompanying a decrease in biodiversity prior to the Late Ordovician Mass Extinction

Xinze Lu, Geoffrey J. Gilleaudeau, Brian Kendall

Summary: The Late Ordovician mass extinction is the first major extinction event in the Phanerozoic, but the reasons for the decline in global biodiversity before the extinction are not well understood.

GEOCHIMICA ET COSMOCHIMICA ACTA (2024)

Article Geochemistry & Geophysics

Trace element evidence for diverse origins of superheavy pyrite in Neoproterozoic sedimentary strata

Junyao Kang, Daniel D. Gregory, Benjamin Gill, Shiqiang Huang, Changxin Lai, Zhaoshan Chang, Huan Cui, Ivan Belousov, Shuhai Xiao

Summary: Sedimentary pyrite is an important geological archive, but it can be altered by diagenetic and hydrothermal processes. This study successfully trained machine learning algorithms to distinguish pyrite origins using trace element data. The approach was validated and applied to identify the origins of pyrite in two sedimentary successions in South China.

GEOCHIMICA ET COSMOCHIMICA ACTA (2024)