Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic

Long-term, high-resolution measurements of environmental variability are sparse in the High Arctic. In the absence of such data, we turn to proxies recorded in the layered skeletons of the long-lived crustose coralline algae Clathromorphum compactum. Annual growth banding in this alga is dependent o...

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Published in:Frontiers in Marine Science
Main Authors: Jessica Gould, Jochen Halfar, Walter Adey, Justin B. Ries
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
Q
Online Access:https://doi.org/10.3389/fmars.2022.900033
https://doaj.org/article/cffbe2487d82408eb579b37ca8e5be75
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spelling ftdoajarticles:oai:doaj.org/article:cffbe2487d82408eb579b37ca8e5be75 2023-05-15T14:29:28+02:00 Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic Jessica Gould Jochen Halfar Walter Adey Justin B. Ries 2022-08-01T00:00:00Z https://doi.org/10.3389/fmars.2022.900033 https://doaj.org/article/cffbe2487d82408eb579b37ca8e5be75 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2022.900033/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2022.900033 https://doaj.org/article/cffbe2487d82408eb579b37ca8e5be75 Frontiers in Marine Science, Vol 9 (2022) coralline algae growth monitoring calcification sea ice proxy high arctic Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2022 ftdoajarticles https://doi.org/10.3389/fmars.2022.900033 2022-12-31T00:53:48Z Long-term, high-resolution measurements of environmental variability are sparse in the High Arctic. In the absence of such data, we turn to proxies recorded in the layered skeletons of the long-lived crustose coralline algae Clathromorphum compactum. Annual growth banding in this alga is dependent on several factors that include temperature, light availability, nutrients, salinity, and calcium carbonate saturation state. It has been observed that growth slows during winter as sunlight reaching the seafloor diminishes due to decreased insolation and the build-up of sea-ice, such that the relationship between sea-ice cover extent and algal growth has allowed for reconstructions of relative sea-ice variability through time. However, recent laboratory work has shown that C. compactum continue growing in complete darkness (sea-ice cover). Therefore, a more complete understanding of algal growth is necessary for the refinement of the sea-ice proxy. Here, we present the results of a ~year-long in-situ growth and environmental monitoring experiment in Arctic Bay, Nunavut, Canada (~73°N) which addresses, for the first time in situ, the gaps in our understanding of growth over an annual cycle in the High Arctic. Algal growth was assessed on a quasi-monthly basis, where specimens were subsampled to quantify monthly extension in the context of ocean temperature and light availability. By measuring extension rate through time, we observed that the algae grew on average 72 µm yr-1, with ~54% of annual growth occurring during the sea-ice free summer months (June-September), ~25% during the winter months (November-April), and ~21% occurring during the transition months of May and October. Although winter growth slowed, we did not observe a consistent cessation of linear extension during low-or no-light months. We posit that substantial growth during the winter months at this latitude is most likely a consequence of the mobilization of stored energy (photosynthate) produced during the photosynthetically active summer months. ... Article in Journal/Newspaper Arctic bay Arctic Nunavut Sea ice Subarctic Directory of Open Access Journals: DOAJ Articles Arctic Nunavut Canada Arctic Bay ENVELOPE(-85.116,-85.116,73.018,73.018) Frontiers in Marine Science 9
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic coralline algae
growth monitoring
calcification
sea ice proxy
high arctic
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
spellingShingle coralline algae
growth monitoring
calcification
sea ice proxy
high arctic
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
Jessica Gould
Jochen Halfar
Walter Adey
Justin B. Ries
Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
topic_facet coralline algae
growth monitoring
calcification
sea ice proxy
high arctic
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
description Long-term, high-resolution measurements of environmental variability are sparse in the High Arctic. In the absence of such data, we turn to proxies recorded in the layered skeletons of the long-lived crustose coralline algae Clathromorphum compactum. Annual growth banding in this alga is dependent on several factors that include temperature, light availability, nutrients, salinity, and calcium carbonate saturation state. It has been observed that growth slows during winter as sunlight reaching the seafloor diminishes due to decreased insolation and the build-up of sea-ice, such that the relationship between sea-ice cover extent and algal growth has allowed for reconstructions of relative sea-ice variability through time. However, recent laboratory work has shown that C. compactum continue growing in complete darkness (sea-ice cover). Therefore, a more complete understanding of algal growth is necessary for the refinement of the sea-ice proxy. Here, we present the results of a ~year-long in-situ growth and environmental monitoring experiment in Arctic Bay, Nunavut, Canada (~73°N) which addresses, for the first time in situ, the gaps in our understanding of growth over an annual cycle in the High Arctic. Algal growth was assessed on a quasi-monthly basis, where specimens were subsampled to quantify monthly extension in the context of ocean temperature and light availability. By measuring extension rate through time, we observed that the algae grew on average 72 µm yr-1, with ~54% of annual growth occurring during the sea-ice free summer months (June-September), ~25% during the winter months (November-April), and ~21% occurring during the transition months of May and October. Although winter growth slowed, we did not observe a consistent cessation of linear extension during low-or no-light months. We posit that substantial growth during the winter months at this latitude is most likely a consequence of the mobilization of stored energy (photosynthate) produced during the photosynthetically active summer months. ...
format Article in Journal/Newspaper
author Jessica Gould
Jochen Halfar
Walter Adey
Justin B. Ries
author_facet Jessica Gould
Jochen Halfar
Walter Adey
Justin B. Ries
author_sort Jessica Gould
title Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
title_short Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
title_full Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
title_fullStr Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
title_full_unstemmed Growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline C. compactum: A year-long in situ experiment in the high arctic
title_sort growth as a function of sea ice cover, light and temperature in the arctic/subarctic coralline c. compactum: a year-long in situ experiment in the high arctic
publisher Frontiers Media S.A.
publishDate 2022
url https://doi.org/10.3389/fmars.2022.900033
https://doaj.org/article/cffbe2487d82408eb579b37ca8e5be75
long_lat ENVELOPE(-85.116,-85.116,73.018,73.018)
geographic Arctic
Nunavut
Canada
Arctic Bay
geographic_facet Arctic
Nunavut
Canada
Arctic Bay
genre Arctic bay
Arctic
Nunavut
Sea ice
Subarctic
genre_facet Arctic bay
Arctic
Nunavut
Sea ice
Subarctic
op_source Frontiers in Marine Science, Vol 9 (2022)
op_relation https://www.frontiersin.org/articles/10.3389/fmars.2022.900033/full
https://doaj.org/toc/2296-7745
2296-7745
doi:10.3389/fmars.2022.900033
https://doaj.org/article/cffbe2487d82408eb579b37ca8e5be75
op_doi https://doi.org/10.3389/fmars.2022.900033
container_title Frontiers in Marine Science
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