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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2,632
1,172
109
3,913
140
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133
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Cumulative views and downloads
(calculated since 04 Feb 2021)
Total article views: 2,673 (including HTML, PDF, and XML)
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Total
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EndNote
1,974
613
86
2,673
140
103
119
HTML: 1,974
PDF: 613
XML: 86
Total: 2,673
Supplement: 140
BibTeX: 103
EndNote: 119
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Total article views: 1,240 (including HTML, PDF, and XML)
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658
559
23
1,240
16
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 3,913 (including HTML, PDF, and XML)
Thereof 3,818 with geography defined
and 95 with unknown origin.
Total article views: 2,673 (including HTML, PDF, and XML)
Thereof 2,619 with geography defined
and 54 with unknown origin.
Total article views: 1,240 (including HTML, PDF, and XML)
Thereof 1,199 with geography defined
and 41 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...