Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front

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Standard

Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front. / Bendtsen, Jørgen; Daugbjerg, Niels; Jensen, Rune Stefan; Brady, Mariska; Nielsen, Morten Holtegaard; Hansen, Jørgen L. S.; Richardson, Katherine.

In: Marine Ecology - Progress Series, Vol. 727, 2024, p. 67-80.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Bendtsen, J, Daugbjerg, N, Jensen, RS, Brady, M, Nielsen, MH, Hansen, JLS & Richardson, K 2024, 'Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front', Marine Ecology - Progress Series, vol. 727, pp. 67-80. https://doi.org/10.3354/meps14489

APA

Bendtsen, J., Daugbjerg, N., Jensen, R. S., Brady, M., Nielsen, M. H., Hansen, J. L. S., & Richardson, K. (2024). Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front. Marine Ecology - Progress Series, 727, 67-80. https://doi.org/10.3354/meps14489

Vancouver

Bendtsen J, Daugbjerg N, Jensen RS, Brady M, Nielsen MH, Hansen JLS et al. Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front. Marine Ecology - Progress Series. 2024;727:67-80. https://doi.org/10.3354/meps14489

Author

Bendtsen, Jørgen ; Daugbjerg, Niels ; Jensen, Rune Stefan ; Brady, Mariska ; Nielsen, Morten Holtegaard ; Hansen, Jørgen L. S. ; Richardson, Katherine. / Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front. In: Marine Ecology - Progress Series. 2024 ; Vol. 727. pp. 67-80.

Bibtex

@article{9da6dcaf98d345559a564382b7741590,
title = "Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front",
abstract = "The main strait (Great Belt) connecting the North Sea and the Baltic Sea constitutes a quasi-stationary front and exposes phytoplankton to various degrees of water column mixing. Here, we examine phytoplankton community distributions (using the cell abundance of 4 readily identifiable diatoms) and estimate new production along the strait during early spring. Vertical turbulent mixing was ~10 times greater at stations in the strait compared to stations outside the strait. New production in the strait was on average ~50 mg C m-2 d-1, i.e. 8% of the average total primary production and could explain the increase in chlorophyll observed along the strait. An NMDS-analysis of phytoplankton community composition showed significant spatial groupings. However, variation of species abundances could not be explained by the general transport, where the abundance of the largest species decreased during the passage of the strait. A relatively small species (Guinardia delicatula) showed an increasing dominance in and above the subsurface chlorophyll maximum along the strait, and the bottom layer was also correspondingly dominated by a relatively small species (Skeletonema marinoi). This phytoplankton composition could be explained by photosynthetic traits associated with more efficient light usage of small cells together with increased nutrient supply in the strait.",
author = "J{\o}rgen Bendtsen and Niels Daugbjerg and Jensen, {Rune Stefan} and Mariska Brady and Nielsen, {Morten Holtegaard} and Hansen, {J{\o}rgen L. S.} and Katherine Richardson",
year = "2024",
doi = "10.3354/meps14489",
language = "English",
volume = "727",
pages = "67--80",
journal = "Marine Ecology - Progress Series",
issn = "0171-8630",
publisher = "Inter-Research",

}

RIS

TY - JOUR

T1 - Phytoplankton community changes in relation to nutrient fluxes along a quasi-stationary front

AU - Bendtsen, Jørgen

AU - Daugbjerg, Niels

AU - Jensen, Rune Stefan

AU - Brady, Mariska

AU - Nielsen, Morten Holtegaard

AU - Hansen, Jørgen L. S.

AU - Richardson, Katherine

PY - 2024

Y1 - 2024

N2 - The main strait (Great Belt) connecting the North Sea and the Baltic Sea constitutes a quasi-stationary front and exposes phytoplankton to various degrees of water column mixing. Here, we examine phytoplankton community distributions (using the cell abundance of 4 readily identifiable diatoms) and estimate new production along the strait during early spring. Vertical turbulent mixing was ~10 times greater at stations in the strait compared to stations outside the strait. New production in the strait was on average ~50 mg C m-2 d-1, i.e. 8% of the average total primary production and could explain the increase in chlorophyll observed along the strait. An NMDS-analysis of phytoplankton community composition showed significant spatial groupings. However, variation of species abundances could not be explained by the general transport, where the abundance of the largest species decreased during the passage of the strait. A relatively small species (Guinardia delicatula) showed an increasing dominance in and above the subsurface chlorophyll maximum along the strait, and the bottom layer was also correspondingly dominated by a relatively small species (Skeletonema marinoi). This phytoplankton composition could be explained by photosynthetic traits associated with more efficient light usage of small cells together with increased nutrient supply in the strait.

AB - The main strait (Great Belt) connecting the North Sea and the Baltic Sea constitutes a quasi-stationary front and exposes phytoplankton to various degrees of water column mixing. Here, we examine phytoplankton community distributions (using the cell abundance of 4 readily identifiable diatoms) and estimate new production along the strait during early spring. Vertical turbulent mixing was ~10 times greater at stations in the strait compared to stations outside the strait. New production in the strait was on average ~50 mg C m-2 d-1, i.e. 8% of the average total primary production and could explain the increase in chlorophyll observed along the strait. An NMDS-analysis of phytoplankton community composition showed significant spatial groupings. However, variation of species abundances could not be explained by the general transport, where the abundance of the largest species decreased during the passage of the strait. A relatively small species (Guinardia delicatula) showed an increasing dominance in and above the subsurface chlorophyll maximum along the strait, and the bottom layer was also correspondingly dominated by a relatively small species (Skeletonema marinoi). This phytoplankton composition could be explained by photosynthetic traits associated with more efficient light usage of small cells together with increased nutrient supply in the strait.

U2 - 10.3354/meps14489

DO - 10.3354/meps14489

M3 - Journal article

VL - 727

SP - 67

EP - 80

JO - Marine Ecology - Progress Series

JF - Marine Ecology - Progress Series

SN - 0171-8630

ER -

ID: 372719772