Total for the last 12 months
number of access : ?
number of downloads : ?
ID 117326
Author
Nakano, Takanori Research Institute for Humanity and Nature
Shin, Ki-Cheol Research Institute for Humanity and Nature
Matsubayashi, Jun Research Institute for Humanity and Nature|Japan Agency for Marine-Earth Science and Technology
Kato, Yoshikazu Research Institute for Humanity and Nature
Amakawa, Hiroshi Japan Agency for Marine-Earth Science and Technology
Osada, Yutaka Research Institute for Humanity and Nature|Tohoku University
Yoshimizu, Chikage Research Institute for Humanity and Nature
Okuda, Noboru Research Institute for Humanity and Nature
Amano, Yosuke Tohoku National Fisheries Research Institute|Fukushima Prefectural Fisheries and Marine Science Research Centre
Togashi, Hiroyuki Tohoku National Fisheries Research Institute
Kurita, Yutaka Tohoku National Fisheries Research Institute
Tayasu, Ichiro Research Institute for Humanity and Nature
Keywords
animal migration
catchment geology
Ce anomaly
coastal sea
mussel
Nd isotope ratio
oyster
river water
seawater
shellfish
tracer
Content Type
Journal Article
Description
Isotopic compositions of animal tissue are an intrinsic marker commonly used to trace animal origins and migrations; however, few isotopes are effective for this purpose in marine environments, especially on a local scale. The isotope ratio of the lanthanoid element neodymium (Nd) is a promising tracer for coastal animal migrations. Neodymium derives from the same geologic materials as strontium, well known as an isotopic tracer (87Sr/86Sr) for terrestrial and anadromous animals. The advantage of the Nd isotope ratio (143Nd/144Nd, expressed as εNd) is that it varies greatly in the ocean according to the geology of the neighboring continents, whereas oceanic 87Sr/86Sr is highly uniform. This study explored the utility of the Nd isotope ratio as a marine tracer by investigating the variation of εNd preserved in tissues of coastal species, and the causes of that variation, in a region of northeastern Japan where the bedrock geology is highly variable. We measured εNd and 87Sr/86Sr in seawater, river water, and soft tissues of sedentary suspension feeders: the mussels Mytilus galloprovincialis and Mytilus coruscus and the oyster Crassostrea gigas. We also measured concentrations of three lanthanoids (La, Ce, and Pr) in shellfish bodies to determine whether the Nd in shellfish tissue was derived from solution in seawater or from suspended particulates. The εNd values in shellfish tissue varied regionally (−6 to +1), matching the ambient seawater, whereas all 87Sr/86Sr values were homogeneous and typical of seawater (0.7091–0.7092). The seawater εNd values were in turn correlated with those in the adjacent rivers, linking shellfish εNd to the geology of river catchments. The depletion of Ce compared to La and Pr (negative Ce anomaly) suggested that the Nd in shellfish was derived from the dissolved phase in seawater. Our results indicate that the distinct Nd isotope ratio derived from local geology is imprinted, through seawater, on the soft tissues of shellfish. This result underscores the potential of εNd as a tracer of coastal marine animals.
Journal Title
Ecosphere
ISSN
21508925
Publisher
Wiley|Ecological Society of America
Volume
9
Issue
8
Start Page
e02365
Published Date
2018-08-20
Rights
This is an open access article under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/3.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
EDB ID
DOI (Published Version)
URL ( Publisher's Version )
FullText File
language
eng
TextVersion
Publisher
departments
Science and Technology