Department of Earth and Environmental Sciences, University of
Milano–Bicocca, CoNISMa
Research Unit of Milano–Bicocca, Piazza della Scienza 4, 20126 Milan, Italy
Department of Earth and Ocean Dynamics, University of Barcelona,
Martí i Franquès s/n, 08028 Barcelona, Spain
Department of Earth and Environmental Sciences, University of
Milano–Bicocca, CoNISMa
Research Unit of Milano–Bicocca, Piazza della Scienza 4, 20126 Milan, Italy
Department of Earth and Environmental Sciences, University of
Milano–Bicocca, CoNISMa
Research Unit of Milano–Bicocca, Piazza della Scienza 4, 20126 Milan, Italy
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2,612
1,158
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3,878
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EndNote: 132
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Cumulative views and downloads
(calculated since 04 Feb 2021)
Total article views: 2,647 (including HTML, PDF, and XML)
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1,957
605
85
2,647
133
100
118
HTML: 1,957
PDF: 605
XML: 85
Total: 2,647
Supplement: 133
BibTeX: 100
EndNote: 118
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655
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Total article views: 3,878 (including HTML, PDF, and XML)
Thereof 3,784 with geography defined
and 94 with unknown origin.
Total article views: 2,647 (including HTML, PDF, and XML)
Thereof 2,593 with geography defined
and 54 with unknown origin.
Total article views: 1,231 (including HTML, PDF, and XML)
Thereof 1,191 with geography defined
and 40 with unknown origin.
The coralline alga Lithothamnion corallioides is widely distributed in the Mediterranean Sea and NE Atlantic Ocean, where it constitutes rhodolith beds, which are diversity-rich ecosystems on the seabed. The boron incorporated in the calcified thallus of coralline algae (B/Ca) can be used to trace past changes in seawater carbonate and pH. This paper suggests a non-negligible effect of algal growth rate on B/Ca, recommending caution in adopting this proxy for paleoenvironmental reconstructions.
The coralline alga Lithothamnion corallioides is widely distributed in the Mediterranean Sea and...
