Reconstruction of the salinity history associated with movements of mangrove fishes using otolith oxygen isotopic analysis

Abstract

MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 593:127-139 (2018) - DOI: https://doi.org/10.3354/meps12514 Reconstruction of the salinity history associated with movements of mangrove fishes using otolith oxygen isotopic analysis Kotaro Shirai1,*, Futa Koyama2, Naoko Murakami-Sugihara1, Kusuto Nanjo3, Tomihiko Higuchi1, Hiroyoshi Kohno4, Yoshiro Watanabe1, Ken Okamoto2, Mitsuhiko Sano2 1Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwanoha, Kashiwa, Chiba 277-8564, Japan 2Department of Ecosystem Studies, Graduate School of Agricultural and Life Sciences, The University of Tokyo, Yayoi, Bunkyo, Tokyo 113-8657, Japan 3Department of Applied Aquabiology, National Fisheries University, Nagata-honmachi, Shimonoseki, Yamaguchi 759-6595, Japan 4Okinawa Regional Research Center, Tokai University, Uehara, Taketomi, Okinawa 907-1541, Japan *Corresponding author: kshirai@aori.u-tokyo.ac.jp ABSTRACT: Recent degradation and loss of tropical estuaries due to human impact have made necessary the protection of essential habitats for estuarine fishes. A better understanding of estuarine use patterns contributes greatly to identifying essential habitat conditions. This study presents quantitative reconstruction data of the salinity history experienced by individual estuarine fishes using an otolith oxygen isotope. δ18Ootolith was determined from the kuhliid Kuhlia rupestris and pomacentrid Chrysiptera cyanea for use as freshwater and marine end-member references, respectively. The salinity histories of 3 species of estuarine mangrove fishes, often dominant in tropical East Asian estuaries, viz. the apogonid Fibramia amboinensis, the pomacentrid Neopomacentrus taeniurus and the terapontid Terapon jarbua, were examined. The δ18Ootolith ranges of -5.4 to -2.3‰ for F. amboinensis and -3.7 to -2.3‰ for N. taeniurus corresponded to 6 to 30 psu and 19 to 30 psu, respectively, when compared to the 2 extreme salinity values of the reference fishes. Terapon jarbua, in contrast, exhibited a δ18Ootolith range of -3.0 to -1.8‰, corresponding to 25 to 34 psu. Field observations in other studies have indicated that F. amboinensis and N. taeniurus may be resident species, hovering near mangrove roots and tolerating a variable salinity environment, whereas T. jarbua may be a vagile species that can move to areas of preferred higher salinity conditions. Such behavioral ecologies are largely consistent with the salinity histories reconstructed from δ18Ootolith data. These results suggest that F. amboinensis and N. taeniurus may be estuarine resident fishes, whereas T. jarbua may be a marine migrant. KEY WORDS:Fibramia amboinensis · Neopomacentrus taeniurus · Terapon jarbua · Estuary · Habitat · Space use · Stable isotope analysis Full text in pdf format Supplementary material PreviousNextCite this article as: Shirai K, Koyama F, Murakami-Sugihara N, Nanjo K and others (2018) Reconstruction of the salinity history associated with movements of mangrove fishes using otolith oxygen isotopic analysis. Mar Ecol Prog Ser 593:127-139. https://doi.org/10.3354/meps12514 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 593. Online publication date: April 12, 2018 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2018 Inter-Research.