Quantifying floridean starch storage patterns in Arctic rhodoliths: blue carbon implications

Rhodoliths composed of crustose coralline algae (CCA) are marine calcifiers of global significance. Here, we investigate how floridean starch storage patterns of Arctic rhodoliths from Svalbard are affected by environmental conditions. Quantifying the amount of starch in photomosaic scans of rhodoli...

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Published in:Polar research Vol. 44; pp. 1 - 14
Main Authors: Gabsteiger, Milane, Pyko, Ines, Wisshak, Max, Teichert, Sebastian
Format: Journal Article
Language:English
Published: Spånga Open Academia 01.09.2025
Norwegian Polar Institute
Subjects:
Algae
Amylopectin
Blue carbon
boreolithothamnion glaciale
Calcification
calcifiers
Carbon
Carbon sinks
Complex formation
crustose coralline algae
depth gradient
Dieback
Environmental conditions
Glucose
Iodine
marine carbon sink
Organisms
Shallow water
Starch
svalbard
Thallus
Water
Water depth
Arctic region
ISSN:0800-0395, 1751-8369
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Abstract Rhodoliths composed of crustose coralline algae (CCA) are marine calcifiers of global significance. Here, we investigate how floridean starch storage patterns of Arctic rhodoliths from Svalbard are affected by environmental conditions. Quantifying the amount of starch in photomosaic scans of rhodolith slabs via amylopectin–iodine complex formation, we found that shallow water rhodoliths contain significantly higher starch percentages compared to the deeper-water dwellers. We conclude that the observed starch patterns are mainly controlled by water depth because light and rhodolith turnover frequency both decrease in deeper waters. Regarding rhodolith turnover, the occasional burial of turned rhodoliths in deeper waters can result in a dieback of the outer CCA thallus areas, which contain important starch supplies. As rhodoliths are both calcifiers and photoautotrophs, we highlight their relevance in potentially contributing to global blue carbon, that is, their role as a marine carbon sink. In this context, our quantification approach of floridean starch patterns in rhodoliths provides a straightforward basis for further studies on this topic.
AbstractList Rhodoliths composed of crustose coralline algae (CCA) are marine calcifiers of global significance. Here, we investigate how floridean starch storage patterns of Arctic rhodoliths from Svalbard are affected by environmental conditions. Quantifying the amount of starch in photomosaic scans of rhodolith slabs via amylopectin–iodine complex formation, we found that shallow water rhodoliths contain significantly higher starch percentages compared to the deeper-water dwellers. We conclude that the observed starch patterns are mainly controlled by water depth because light and rhodolith turnover frequency both decrease in deeper waters. Regarding rhodolith turnover, the occasional burial of turned rhodoliths in deeper waters can result in a dieback of the outer CCA thallus areas, which contain important starch supplies. As rhodoliths are both calcifiers and photoautotrophs, we highlight their relevance in potentially contributing to global blue carbon, that is, their role as a marine carbon sink. In this context, our quantification approach of floridean starch patterns in rhodoliths provides a straightforward basis for further studies on this topic.
Author Wisshak, Max
Gabsteiger, Milane
Teichert, Sebastian
Pyko, Ines
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– volume: 9
  year: 2020
  ident: CIT0031
  publication-title: Plants
  doi: 10.3390/plants9091089
– year: 1988
  ident: CIT0057
  publication-title: The coralline red algae
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Snippet Rhodoliths composed of crustose coralline algae (CCA) are marine calcifiers of global significance. Here, we investigate how floridean starch storage patterns...
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SubjectTerms Algae
Amylopectin
Blue carbon
boreolithothamnion glaciale
Calcification
calcifiers
Carbon
Carbon sinks
Complex formation
crustose coralline algae
depth gradient
Dieback
Environmental conditions
Glucose
Iodine
marine carbon sink
Organisms
Shallow water
Starch
svalbard
Thallus
Water
Water depth
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Title Quantifying floridean starch storage patterns in Arctic rhodoliths: blue carbon implications
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