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  4. Ontogenetic vertical migration of grenadiers revealed by otolith microstructures and stable isotopic composition
 
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Ontogenetic vertical migration of grenadiers revealed by otolith microstructures and stable isotopic composition

Resource
Deep Sea Research Part I: Oceanographic Research Papers, 61, 123-130
Journal
Deep-Sea Research Part I: Oceanographic Research Papers
Journal Volume
61
Pages
123-130
Date Issued
2012
Author(s)
YUE-GAU CHEN  
Lin, Hsien-Yung
Lin, Hsien-Yung
JEN-CHIEH SHIAO  
Shiao, Jen-Chieh  
Chen, Yue-Gau  
Iizuka, Yoshiyuki
DOI
10.1016/j.dsr.2011.12.005
URI
http://www.scopus.com/inward/record.url?eid=2-s2.0-84862807667&partnerID=MN8TOARS
http://scholars.lib.ntu.edu.tw/handle/123456789/370716
Abstract
Otolith δ18O and δ13C of six species grenadiers were analyzed to reconstruct the historical residing depths and metabolic activity. During the larval to juvenile stage, Spicomacrurus kuronumai, Hymenocephalus lethonemus, and Bathygadus nipponicus gradually migrated from the mixed layer to the thermocline downward over a vertical distance >140m after which they moved within a narrow vertical range for the remaining life. The downward migration distance was less than 65m during the larval stage of Hymenocephalus sp. and Coryphaenoides acrolepis, which showed a second descent period from the thermocline to deeper water as juveniles. Coryphaenoides marginatus stayed at the lower thermocline during the larval stage and the juveniles migrated downward in a relative short distance around 100m and settled in deeper water (>600m), followed by irregular movements over a vertical range of about 200m during juvenile and adult stages. The otolith δ13C profile suggested that fishes (S. kuronumai, H. lethonemus, and B. nipponicus) with a longer migration distance had a higher metabolic rate in their early life-history stages than in the later stages. However, the metabolic rate did not vary for those fishes (H. sp., C. acrolepis and C. marginatus) living within a narrow vertical range during their larval to adult stages. The otolith microchemistry suggested that ontogenetic downward migration was an important strategy for grenadiers linking the life stages between pelagic larvae and benthic settlement. Furthermore, the migration timing and distance for the pelagic larvae varied between species and habitats. S. kuronumai, H. lethonemus, H. sp. and C. acrolepis might metamorphose and settle at the same time, B. nipponicus metamorphosed during migration and C. marginatus migrated as juveniles. © 2011 Elsevier Ltd.
Subjects
Grenadiers; Life history; Ontogenetic vertical migration; Otolith stable isotope
SDGs

[SDGs]SDG14

Other Subjects
Fish; Isotopes; Metabolism; Grenadiers; Life history; Metabolic activity; Metabolic rates; Migration distance; Ontogenetic vertical migrations; Stable isotopes; Stable isotopic compositions; Stream flow; benthos; deep water; fish; isotopic composition; larval settlement; life history; marine ecosystem; metabolism; microstructure; migratory behavior; migratory species; ontogeny; otolith; thermocline; vertical migration; Bathygadus nipponicus; Coryphaenoides acrolepis; Coryphaenoides marginatus; Hymenocephalus; Macrouridae; Pisces
Type
journal article

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