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Effect of diet isotopic ratios on the \(\mathsf{\delta^{13}C}\) and \(\mathsf{\delta^{15}N}\) signatures of scallop-gut contents in a natural setting

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www.jstage.jst.go.jp
Date
2023
Author
Aya, Frolan ORCID
Kudo, Isao ORCID
Page views
411
ASFA keyword
growth ASFA
nitrogen isotopes ASFA
scallop culture ASFA
AGROVOC keyword
scallops AGROVOC
diet quality AGROVOC
Taxonomic term
Mizuhopecten yessoensis GBIF
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Abstract
The relationship between diet isotopic signatures and the extent of the tissue-diet isotope fractionation factors have been shown previously in controlled feeding studies, but this relationship remains poorly resolved for marine invertebrates in a natural setting. Using isotope analysis of gut contents, this study investigated the variability in tissue-diet isotopic fractionation factors (Δδ13C and Δδ15N) between scallop tissues (i.e. muscle and digestive gland) and gut content in the Japanese scallop Mizuhopecten yessoensis (Jay, 1857) and assessed how the growth rate of juvenile scallops and gut content quality (as carbon to nitrogen (C/N) molar ratios) would affect the values of tissue-diet isotopic fractionation. Tissue-diet isotopic fractionation factors (Δδ13C and δ15N) varied according to tissue, which averaged 1.7‰ and −0.1‰ for N in muscle and digestive gland, and 3.4‰ and 1.2‰ for C in muscle and digestive gland, respectively. Muscle-gut δ15N isotopic factors negatively correlated with growth rate, suggesting that the juvenile δ15N signatures were strongly dependent on food quantity. The influence of diet quality on δ15N was also evident, where δ15N decreased as C/N molar ratios in gut contents increased. The wide difference in Δδ13C and δ15N from accepted standard values may be, in part, a consequence of using gut contents as a dietary proxy. Results of this study have implications for diet reconstruction studies of this scallop species reared under field conditions.
Keywords
growth diet composition Mizuhopecten yessoensis stable carbon and nitrogen isotopes tissue-diet isotopic fractionation Japanese scallop Ezo giant scallop
URI
http://hdl.handle.net/10862/6475
Suggested Citation
Aya, F., & Kudo, I. (2023). Effect of diet isotopic ratios on the \(\mathsf{\delta^{13}C}\) and \(\mathsf{\delta^{15}N}\) signatures of scallop-gut contents in a natural setting. Plankton and Benthos Research, 18(3), 140-147. https://doi.org/10.3800/pbr.18.140 
DOI
10.3800/pbr.18.140
Type
Article
ISSN
1880-8247; 1882-627X
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  • Journal Articles [1267]

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    Seasonal growth, organ indices and food consumption of the Japanese scallop Patinopecten yessoensis (Jay, 1857) in relation to food availability in Tokoro seabed, Okhotsk Sea, North Japan 

    Aya, Frolan ORCID; Kudo, Isao ORCID (The Plankton Society of Japan (The Japanese Association of Benthology), 2022-05-30)
    The coastal waters off Tokoro, Okhotsk Sea have been characterized by a substantial decrease in primary production from spring to summer season which will have repercussions on the maintenance of the Japanese scallop Patinopecten yessoensis (Jay, 1857) culture. This study examined the seasonal changes in scallop growth, condition and organ indices in relation to environmental conditions, and compared the sinking particulate organic carbon (POC) flux as an estimate of food availability to scallop food requirements. Monthly specimens were obtained in July 2005, and from May 2006 to December 2008 off Tokoro, Okhotsk Sea. Growth parameters derived from the modified von Bertalanffy growth function of 885 scallop individuals were the mean asymptotic shell height H∞=126.51 mm, Brody growth coefficient K=0.081 year−1, and t0=6.19 year. Condition (CI) and gonadosomatic indices (GSI) increased in April and May, decreased from June to September, but increased again from October until May. The adductor muscle index (AMI) increased from June to October, but declined from November until May when CI and GSI began to increase. Primary production (PP) and chlorophyll a biomass decreased from spring (25.75–29.74 µg C L−1 h−1 and 1.74–5.37 µg L−1) to autumn (0.90–10.83 µg C L−1 h−1 and 0.29–0.75 µg L−1) concurrent with decreasing CI and GSI, but no deleterious effect on AMI was evident during these periods. The sinking POC flux (25–68 mg C m−2 day−1) was low during summer when gonad activity was also low, but started to increase in autumn when gonad activity started to peak. Although a deficit in food availability (lower sinking POC fluxes than scallop food consumption) was observed during summer, the potential advection of organic matter from offshore to nearshore region may have provided additional source of food to bottom-cultured scallops, contributing in part to the increase in shell growth and somatic tissues.
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    Diet-tissue stable isotopic fractionation of tropical sea cucumber, Holothuria scabra 

    Watanabe, Satoshi; Kodama, Masashi; Sumbing, Joemel Gentelizo; Lebata-Ramos, Maria Junemie Hazel ORCID (Japan International Research Center for Agricultural Sciences (JIRCAS), 2013)
    To provide a basis for a stable carbon and nitrogen isotope ratio \(\mathsf{(\delta^{13}C / \delta^{15}N)}\) analysis to determine the assimilated organic matter in sea cucumber, Holothuria scabra, diet-tissue fractionations were experimentally determined by mono-feeding rearing with diatom. While δ15N fractionation of the whole body wall (2.4‰) was similar to the commonly accepted value (2.6 - 4‰), δ13C fractionation of the body wall (4.2‰) showed considerable discrepancy with the commonly accepted value (0 - 1‰) due to the high content (35% dry wt/wt) of calcareous spicules (CaCO3) in the body wall, which had significantly higher δ13C (-8.6‰) than the organic fractions. Computational elimination of spicules based upon spicule content and spicule δ13C reduced the δ13C fractionation of the body wall to 1.5‰, close to the common value. δ13C fractionation after spicule removal by acid decarbonation and subsequent rinsing (3.2‰) did not agree with the common value, and δ15N fractionation was significantly elevated by decarbonation. δ15N and δ13C fractionations of the intestine (1.5 and 2.2‰, respectively) did not agree with the common values. Since δ13C and δ15N of the feces did not differ significantly from those of the diet, feces may be used to determine ingested organic matter in the wild.
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    Stable carbon and nitrogen isotope ratios of penaeid juveniles and primary producers in a riverine mangrove in Guimaras, Philippines 

    Primavera, Jurgenne ORCID (University of Miami, Rosenstiel School of Marine and Atmospheric Science, 1996)
    Stable carbon and nitrogen isotope ratios were analyzed for primary producers and juveniles of four penaeid species (Metapenaeus ensis, Penaeus indicus, P. merquiensi and P. monodon) in a riverine mangrove in Guimaras, central Philippines. δ13C values of shrimp (- 15.5 to - 19.6‰) were closer to phytoplankton (-23.8‰) and possibly epiphytic algae (-24.2‰) than to mangrove leaves (-26.9 to -30.0‰) or detritus (-28.0‰). Differences in δ15N values suggested 2-3 trophic shifts between phytoplankton (0.6‰) and shrimp (6.9‰), assuming a 2.4‰ enrichment per trophic level. There were no significant differences in δ13C and δ15N ratios between green and decomposing leaves, and among mangrove species, shrimp species and different size groups of shrimp.

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