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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2,485
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3,689
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Cumulative views and downloads
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Total article views: 2,501 (including HTML, PDF, and XML)
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1,863
560
78
2,501
117
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HTML: 1,863
PDF: 560
XML: 78
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Supplement: 117
BibTeX: 91
EndNote: 108
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622
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Total article views: 3,689 (including HTML, PDF, and XML)
Thereof 3,588 with geography defined
and 101 with unknown origin.
Total article views: 2,501 (including HTML, PDF, and XML)
Thereof 2,440 with geography defined
and 61 with unknown origin.
Total article views: 1,188 (including HTML, PDF, and XML)
Thereof 1,148 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...