An annual cycle of diatom succession in two contrasting Greenlandic fjords: from simple sea-ice indicators to varied seasonal strategists
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An annual cycle of diatom succession in two contrasting Greenlandic fjords : from simple sea-ice indicators to varied seasonal strategists. / Luostarinen, Tiia; Ribeiro, Sofia; Weckström, Kaarina; Sejr, Mikael; Meire, Lorenz; Tallberg, Petra; Heikkilä, Maija.
I: Marine Micropaleontology, Bind 158, 101873, 2020.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - An annual cycle of diatom succession in two contrasting Greenlandic fjords
T2 - from simple sea-ice indicators to varied seasonal strategists
AU - Luostarinen, Tiia
AU - Ribeiro, Sofia
AU - Weckström, Kaarina
AU - Sejr, Mikael
AU - Meire, Lorenz
AU - Tallberg, Petra
AU - Heikkilä, Maija
N1 - Funding Information: This study was funded by the Academy of Finland (project no. 307282 and no. 296895) and GEOCENTER Danmark (project GreenShift). The time series data were collected by the MarineBasis–Zackenberg marine climate monitoring programme, and MarineBasis Nuuk monitoring program, part of Greenland Ecosystem Monitoring programme (g-e-m.dk). L.M. was funded by research programme VENI with project number 016.Veni.192.150 from the Dutch Research Council (NWO). We thank editors and two anonymous reviewers for their comments that greatly improved the manuscript. We also thank Annette Ryge, Charlotte Olsen, Kitte Linding Gerlich, Heini Ali-Kovero and Meeri Näppilä for help with the sample preparation and analyses. We acknowledge the use of imagery from the NASA Worldview application (https://worldview.earthdata.nasa.gov), part of the NASA Earth Observing System Data and Information System (EOSDIS). Funding Information: This study was funded by the Academy of Finland (project no. 307282 and no. 296895 ) and GEOCENTER Danmark (project GreenShift). The time series data were collected by the MarineBasis–Zackenberg marine climate monitoring programme, and MarineBasis Nuuk monitoring program, part of Greenland Ecosystem Monitoring programme (g-e-m.dk). L.M. was funded by research programme VENI with project number 016.Veni.192.150 from the Dutch Research Council (NWO). We thank editors and two anonymous reviewers for their comments that greatly improved the manuscript. We also thank Annette Ryge, Charlotte Olsen, Kitte Linding Gerlich, Heini Ali-Kovero and Meeri Näppilä for help with the sample preparation and analyses. We acknowledge the use of imagery from the NASA Worldview application ( https://worldview.earthdata.nasa.gov ), part of the NASA Earth Observing System Data and Information System (EOSDIS). Publisher Copyright: © 2020 Elsevier B.V.
PY - 2020
Y1 - 2020
N2 - We recorded diatom species succession over one full year (May 2017–May 2018) using automated sediment traps installed in two contrasting Greenlandic fjords: the seasonally ice-covered Young Sound in high-arctic Northeast Greenland and the nearly sea-ice free Godthåbsfjord in subarctic Southwest Greenland. The traps were positioned at differing water depths (37 m in Young Sound vs. 300 m in Godthåbsfjord). Distinct differences between the study sites were observed in both sediment and diatom fluxes. In Young Sound, total diatom flux was extremely seasonal and as high as 880 × 106 valves m−2 d−1 in the spring. In Godthåbsfjord, total diatom flux was more stable throughout the year, with a maximum of 320 × 106 valves m−2 d−1 in the summer. The diatom assemblage in Young Sound was dominated by the sea-ice species Fragilariopsis oceanica, Fragilariopsis reginae-jahniae and Fossula arctica, which exhibited pulse-like deposition in the trap during and after the ice melt. In Godthåbsfjord, the fluxes were dominated by Chaetoceros (resting spores), while the remaining assemblage was characterised by the cold-water indicator species Detonula confervacea (resting spores) and Thalassiosira antarctica var. borealis (resting spores) together with Fragilariopsis cylindrus. Our data show that, F. oceanica, F. reginae-jahniae and F. arctica exhibit similar seasonal behaviour and a clear link to sea ice. Fragilariopsis cylindrus seems to have a more flexible niche, and based on our study, cannot be considered an unequivocal ice indicator. Taking into account these ecological and seasonal preferences of individual diatom species is crucial when reconstructing past sea-ice conditions both qualitatively and quantitatively.
AB - We recorded diatom species succession over one full year (May 2017–May 2018) using automated sediment traps installed in two contrasting Greenlandic fjords: the seasonally ice-covered Young Sound in high-arctic Northeast Greenland and the nearly sea-ice free Godthåbsfjord in subarctic Southwest Greenland. The traps were positioned at differing water depths (37 m in Young Sound vs. 300 m in Godthåbsfjord). Distinct differences between the study sites were observed in both sediment and diatom fluxes. In Young Sound, total diatom flux was extremely seasonal and as high as 880 × 106 valves m−2 d−1 in the spring. In Godthåbsfjord, total diatom flux was more stable throughout the year, with a maximum of 320 × 106 valves m−2 d−1 in the summer. The diatom assemblage in Young Sound was dominated by the sea-ice species Fragilariopsis oceanica, Fragilariopsis reginae-jahniae and Fossula arctica, which exhibited pulse-like deposition in the trap during and after the ice melt. In Godthåbsfjord, the fluxes were dominated by Chaetoceros (resting spores), while the remaining assemblage was characterised by the cold-water indicator species Detonula confervacea (resting spores) and Thalassiosira antarctica var. borealis (resting spores) together with Fragilariopsis cylindrus. Our data show that, F. oceanica, F. reginae-jahniae and F. arctica exhibit similar seasonal behaviour and a clear link to sea ice. Fragilariopsis cylindrus seems to have a more flexible niche, and based on our study, cannot be considered an unequivocal ice indicator. Taking into account these ecological and seasonal preferences of individual diatom species is crucial when reconstructing past sea-ice conditions both qualitatively and quantitatively.
KW - Arctic
KW - Diatom
KW - Fjord
KW - Godthåbsfjord
KW - Northeast Greenland
KW - Palaeoceanography
KW - Sea ice
KW - Seasonal
KW - Sediment trap
KW - Southwest Greenland
KW - Young Sound
U2 - 10.1016/j.marmicro.2020.101873
DO - 10.1016/j.marmicro.2020.101873
M3 - Journal article
AN - SCOPUS:85086827913
VL - 158
JO - Marine Micropaleontology
JF - Marine Micropaleontology
SN - 0377-8398
M1 - 101873
ER -
ID: 362324853