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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2,560
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3,797
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127
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Cumulative views and downloads
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Total article views: 2,589 (including HTML, PDF, and XML)
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1,924
581
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2,589
127
98
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HTML: 1,924
PDF: 581
XML: 84
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Supplement: 127
BibTeX: 98
EndNote: 115
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636
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Total article views: 3,797 (including HTML, PDF, and XML)
Thereof 3,698 with geography defined
and 99 with unknown origin.
Total article views: 2,589 (including HTML, PDF, and XML)
Thereof 2,529 with geography defined
and 60 with unknown origin.
Total article views: 1,208 (including HTML, PDF, and XML)
Thereof 1,169 with geography defined
and 39 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...
