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Carbon flux of trophic-functional groups within the colonization process of biofilm-dwelling ciliates in marine ecosystems

Published online by Cambridge University Press:  11 March 2016

Zhongwen Yang
Affiliation:
Laboratory of Microbial Ecology, Ocean University of China, Qingdao 266003, China College of Ocean and Earth Sciences, Xiamen University, Xiamen 361005, China
Yuping Xu
Affiliation:
Laboratory of Microbial Ecology, Ocean University of China, Qingdao 266003, China
Guangjian Xu
Affiliation:
Laboratory of Microbial Ecology, Ocean University of China, Qingdao 266003, China
Henglong Xu*
Affiliation:
Laboratory of Microbial Ecology, Ocean University of China, Qingdao 266003, China
*
Correspondence should be addressed to:H. Xu, Laboratory of Microbial Ecology, Ocean University of China, Qingdao 266003, China email: henglongxu@126.com
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Abstract

Biofilm-dwelling ciliates are a primary component of a biofilm, and play an important role in the functioning of microbial food webs by mediating carbon and energy flux into benthos from plankton. The carbon flux of biofilm-dwelling ciliates was studied at different trophic-functional levels within the colonization process in coastal waters of the Yellow Sea, northern China from May to June 2015. Samples were collected, using a glass slide method, at the time intervals of 1, 3, 7, 10, 14, 21 and 28 days from depths of 1 and 3 m. The carbon biomass of both total ciliates and all trophic-functional groups increased following the logistic growth curve model. During the whole colonization period, the bacterivores and non-selectives were generally the primary contributor to the carbon flux in young samples (<14 days), while the algivores and raptors predominated mature samples (14–28 days) at both depths. In terms of mature samples, however, the non-selectives and algivores were the primary contributors at a depth of 1 m, while the raptors accounted for primary contributions to the carbon flux at a depth of 3 m. Although the times to 50% maximum carbon biomasses were generally ranged 24 days at both depths, the maximum carbon biomasses were significantly higher at depth of 3 m than at 1 m. These results may provide useful information for ecological research on carbon flux from plankton to benthos in marine ecosystems.

Information

Type
Research Article
Copyright
Copyright © Marine Biological Association of the United Kingdom 2016 
Figure 0

Fig. 1. Map showing the study area, which was located in the coastal waters of the Yellow Sea, northern China.

Figure 1

Fig. 2. Colonization dynamics of biomass of total biofilm-dwelling ciliates collected at depths of 1 (A) and 3 m (B) in the coastal waters of the Yellow Sea, northern China, during the study period.

Figure 2

Fig. 3. Colonization dynamics of biomass of four functional groups of biofilm-dwelling ciliate communities collected at depths of 1 m (A–D) and 3 m (E–H) in the coastal waters of the Yellow Sea, northern China, during the study period. B, bacterivores; A, algivores; R, raptors; N, non-selectives.

Figure 3

Table 1. Parameters of increase curves of carbon flux fitness to the logistic model for each trophic-functional group of biofilm-dwelling ciliate communities at depths of 1 and 3 m in coastal waters of the Yellow Sea.

Figure 4

Fig. 4. Temporal variations of relative biomass of four functional groups of biofilm-dwelling ciliates communities collected at two depths of 1 (A) and 3 m (B) in the coastal waters of the Yellow Sea, northern China, during the study period.

Figure 5

Fig. 5. Distance-based redundancy analysis (dbRDA) on Bray–Curtis similarities for the average species-biomass data of heterotrophs (A) and photoautotrophs (B) in 14 samples from depths of 1 and 3 m during the study period, respectively; and correlations of species numbers of four functional groups with the two dbRDA axes.