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Different responses of phytoplankton to Fe manipulation in Fe-limited waters with contrasting surface mixed layer depths in the western subarctic Pacific

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Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/92661

Title: Different responses of phytoplankton to Fe manipulation in Fe-limited waters with contrasting surface mixed layer depths in the western subarctic Pacific
Authors: Yoshida, Kazuhiro Browse this author →KAKEN DB
Nishioka, Jun Browse this author →KAKEN DB
Yasuda, Ichiro Browse this author →KAKEN DB
Suzuki, Koji Browse this author →KAKEN DB
Keywords: Fe-light co-limitation
Vertical mixing
On-deck Fe-manipulation experiment
Phytoplankton photophysiology
Scanning electron microscopy
Issue Date: 15-Jun-2023
Publisher: Springer
Journal Title: Journal of oceanography
Volume: 79
Issue: 5
Start Page: 483
End Page: 497
Publisher DOI: 10.1007/s10872-023-00692-7
Abstract: In the western subarctic Pacific (WSP), iron (Fe) can enhance the biological carbon pump by stimulating phytoplankton photosynthesis. However, little is known about how Fe and light availability controls the phytoplankton photophysiology in the WSP near the Kuril Islands, where water mixing is sometimes enhanced, even in summer. Here, we conducted on-deck Fe-manipulated incubation experiments at two stations where surface mixed layer depths were distinct but showed similar initial macronutrient and dissolved Fe concentrations and phytoplankton community composition even experienced light availability for phytoplankton in the water column could be different. An Fe addition to water samples from the deeper surface-mixed layer enhanced the phytoplankton biomass and the photosynthetic competence in photosystem II (F-v/F-m), suggesting an Fe-light co-limitation, which was supported by the results from high functional absorption cross section of photosystem II (sigma(PSII)) and low light saturation index (E-k). At the shallower mixed layer station, Fe amendment did not stimulate phytoplankton biomass and photosynthesis, indicating that Fe was sufficient for the phytoplankton. Although the centric diatom Chaetoceros species were predominant at both stations throughout incubation, the pennate diatoms Pseudo-nitzschia spp. and Cylindrotheca closterium significantly increased at the deeper and shallower-mixed layer stations, respectively, after Fe enrichment. The elongation of the pennate diatom Neodenticula seminae chains was observed under low Fe availability caused by a chelator. This could be related to the fact that N. seminae is abundant in sediment trap samples from the WSP under Fe-limited conditions and contributed to the high biological pump efficiency.
Rights: This version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature’s AM terms of use, but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: http://dx.doi.org/10.1007/s10872-023-00692-7
Type: article (author version)
URI: http://hdl.handle.net/2115/92661
Appears in Collections:環境科学院・地球環境科学研究院 (Graduate School of Environmental Science / Faculty of Environmental Earth Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: 鈴木 光次

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