dc.contributor.author | Walker, Emily-Zoe Elizabeth | |
dc.contributor.author | Wiedmann, Ingrid | |
dc.contributor.author | Nikolopoulos, Anna | |
dc.contributor.author | Skardhamar, Jofrid | |
dc.contributor.author | Jones, Elizabeth Marie | |
dc.contributor.author | Renner, Angelika | |
dc.date.accessioned | 2022-06-03T08:27:06Z | |
dc.date.available | 2022-06-03T08:27:06Z | |
dc.date.issued | 2022-05-13 | |
dc.description.abstract | Marine ecosystems, and particularly fjords, are experiencing an increasing level of human activity on a yearround basis, including the poorly studied winter period. To improve the knowledge base for environmentally
sustainable management in all seasons, this study provides hydrographic and biological baseline data for the
sub-Arctic fjord Kaldfjorden, Northern Norway (69.7 N, 18.7 E), between autumn 2017 and spring 2018.
Field observations are integrated with results of a numerical ocean model simulation, illustrating how pelagic
biomass, represented by chlorophyll a (Chl a), particulate organic carbon (POC), and zooplankton, is affected
by stratification and circulation from October to May. We observed an unusually warm autumn that likely
delayed the onset of cooling and may have supported the high abundances of holoplankton and meroplankton
(5768 individuals m<sup>–3</sup>). With the onset of winter, the water column cooled and became vertically mixed, while
suspended Chl a concentrations declined rapidly (< 0.12 mg Chl a m<sup>–3</sup>). In January and February, suspended POC
concentrations and downward flux were elevated near the seafloor. The hydrodynamic model results indicate
that the strongest currents at depth occurred in these months, potentially inducing resuspension events close
to the seafloor. In spring (April), peak abundances of suspended biomass were observed (6.9–7.2 mg Chl a m<sup>–3</sup>
at 5–15 m; 9952 zooplankton ind. m<sup>–3</sup> at 0–100 m), and field observations and model results suggest that
zooplankton of Atlantic origin were probably advected into Kaldfjorden. During all investigated seasons, the
model simulation suggests a complex circulation pattern, even in such a small fjord, which can have
implications for environmental management of the fjord. We conclude that the pelagic system in
Kaldfjorden changes continually from autumn to spring and that winter must be seen as a dynamic period,
not a season where the fjord ecosystem is ‘at rest’. | en_US |
dc.identifier.citation | Walker, Wiedmann, Nikolopoulos, Skardhamar, Jones, Renner. Pelagic ecosystem dynamics between late autumn and the post spring bloom in a sub-Arctic fjord. Elementa: Science of the Anthropocene. 2022 | en_US |
dc.identifier.cristinID | FRIDAID 2029144 | |
dc.identifier.doi | 10.1525/elementa.2021.00070 | |
dc.identifier.issn | 2325-1026 | |
dc.identifier.uri | https://hdl.handle.net/10037/25366 | |
dc.language.iso | eng | en_US |
dc.publisher | University of California Press | en_US |
dc.relation.journal | Elementa: Science of the Anthropocene | |
dc.relation.projectID | info:eu-repo/grantAgreement/EC/SOCIETAL CHALLENGES/869383/EU/Arctic biodiversity change and its consequences: Assessing, monitoring and predicting the effects of ecosystem tipping cascades on marine ecosystem services and dependent human systems/ECOTIP/ | en_US |
dc.rights.accessRights | openAccess | en_US |
dc.rights.holder | Copyright 2022 The Author(s) | en_US |
dc.title | Pelagic ecosystem dynamics between late autumn and the post spring bloom in a sub-Arctic fjord | en_US |
dc.type.version | publishedVersion | en_US |
dc.type | Journal article | en_US |
dc.type | Tidsskriftartikkel | en_US |
dc.type | Peer reviewed | en_US |