Vol. 62, 2023
(update: 2023.12.29)
Effects of Tropical Cyclone
Passage on Plankton Community Respiration in a Phosphate-Limited
Freshwater Ecosystem
Erica Silk P. dela Paz1, Chao-Chen Lai2, Fuh-Kwo Shiah3, Chih-hao Hsieh3,4,5, Chia-Ying Ko1,5,*
doi:10.6620/ZS.2023.62-58
1Institute of Fisheries Science, National Taiwan University, Taipei, 106 Taiwan. *Correspondence: E-mail: cyko235@ntu.edu.tw (Ko)
E-mail: d07b45003@ntu.edu.tw (dela Paz)
2Department
of Science Education, National Taipei University of Education, Taipei
106, Taiwan. E-mail: ccjosephlai@mail.ntue.edu.tw (Lai)
3Research Center for Environmental Changes, Academia Sinica, Taipei 115, Taiwan. E-mail: fkshiah@gate.sinica.edu.tw (Shiah)
4Institute of Oceanography, National Taiwan University, Taipei 106, Taiwan. E-mail: chsieh@ntu.edu.tw (Hsieh)
5Master’s Program in Biodiversity, Institute of Ecology and Evolutionary Biology, National Taiwan University, Taipei, 106 Taiwan
(Received 22 August 2023 / Accepted 22
November 2023 / Published 29 December 2023)
Communicated by Benny K.K. Chan
Plankton community respiration (CR)
in aquatic ecosystems varies with environmental factors, which could be
altered during tropical cyclones (TCs). A potential increase in CR
resulting from the effects of TCs is generally understudied. Here, we
examined the relationship between plankton CR and environmental
factors, including during TC-affected periods, in a phosphate-limited
freshwater ecosystem. We conducted an intensive in situ sampling in Fei-Tsui
Reservoir (FTR) from January 2010 to December 2015 during TC periods
and non-TC periods. Our results showed a consistent temporal pattern
that plankton CR increased between March to October and declined
between November to February. These changes in plankton CR, primarily
supported by bacterial biomass, were positively influenced by euphotic
depth-averaged temperature. The CR also significantly increased with
euphotic depth-averaged NO2- concentrations and
decreased with euphotic depth-averaged NO3-
concentrations. These results indicated that these factors typically
influenced CR dynamics in the FTR. During TC periods, plankton CR was
increased further due to a higher and ideal euphotic depth-averaged
temperature (23–27°C) and increased supply of limiting nutrient
resources via stream runoff. Overall, this study showed that a TC
positively influences plankton CR by creating favorable water
conditions. Notably, with a higher frequency of intense TCs projected
for the Western North Pacific in most climate change scenarios, the
impact of TCs on CR may increase in the near future.
Key words: Bacterial biomass, Total
community respiration, Oligotrophic lake, Plankton, Typhoon
Citation:
dela Paz ESP, Lai CC, Shiah FK, Hsieh Ch, Ko CY. 2023. Effects of
tropical cyclone passage on plankton community respiration in a
phosphate-limited freshwater ecosystem. Zool Stud 62:58. doi:10.6620/ZS.2023.62-58.
Supplementary Materials: Fig. S1丨Fig. S2丨Table S1丨Table S2
|