Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.

We developed a geochemical atlas of the Colorado River in Grand Canyon and in its tributary, the Little Colorado River, and used it to identify provenance and habitat use by Federally Endangered humpback chub, Gila cypha. Carbon stable isotope ratios (δ(13)C) discriminate best between the two rivers...

Full description

Bibliographic Details
Main Authors: Karin E Limburg, Todd A Hayden, William E Pine, Michael D Yard, Reinhard Kozdon, John W Valley
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2013-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3865257?pdf=render
id doaj-79818e3cad39461b92a68ca2fe546f94
record_format Article
spelling doaj-79818e3cad39461b92a68ca2fe546f942020-11-24T21:43:49ZengPublic Library of Science (PLoS)PLoS ONE1932-62032013-01-01812e8423510.1371/journal.pone.0084235Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.Karin E LimburgTodd A HaydenWilliam E PineMichael D YardReinhard KozdonJohn W ValleyWe developed a geochemical atlas of the Colorado River in Grand Canyon and in its tributary, the Little Colorado River, and used it to identify provenance and habitat use by Federally Endangered humpback chub, Gila cypha. Carbon stable isotope ratios (δ(13)C) discriminate best between the two rivers, but fine scale analysis in otoliths requires rare, expensive instrumentation. We therefore correlated other tracers (SrSr, Ba, and Se in ratio to Ca) to δ(13)C that are easier to quantify in otoliths with other microchemical techniques. Although the Little Colorado River's water chemistry varies with major storm events, at base flow or near base flow (conditions occurring 84% of the time in our study) its chemistry differs sufficiently from the mainstem to discriminate one from the other. Additionally, when fish egress from the natal Little Colorado River to the mainstem, they encounter cold water which causes the otolith daily growth increments to decrease in size markedly. Combining otolith growth increment analysis and microchemistry permitted estimation of size and age at first egress; size at first birthday was also estimated. Emigrants < 1 year old averaged 51.2 ± 4.4 (SE) days and 35.5 ± 3.6 mm at egress; older fish that had recruited to the population averaged 100 ± 7.8 days old and 51.0 ± 2.2 mm at egress, suggesting that larger, older emigrants recruit better. Back-calculated size at age 1 was unimodal and large (78.2 ± 3.3 mm) in Little Colorado caught fish but was bimodally distributed in Colorado mainstem caught fish (49.9 ± 3.6 and 79 ± 4.9 mm) suggesting that humpback chub can also rear in the mainstem. The study demonstrates the coupled usage of the two rivers by this fish and highlights the need to consider both rivers when making management decisions for humpback chub recovery.http://europepmc.org/articles/PMC3865257?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Karin E Limburg
Todd A Hayden
William E Pine
Michael D Yard
Reinhard Kozdon
John W Valley
spellingShingle Karin E Limburg
Todd A Hayden
William E Pine
Michael D Yard
Reinhard Kozdon
John W Valley
Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
PLoS ONE
author_facet Karin E Limburg
Todd A Hayden
William E Pine
Michael D Yard
Reinhard Kozdon
John W Valley
author_sort Karin E Limburg
title Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
title_short Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
title_full Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
title_fullStr Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
title_full_unstemmed Of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in Grand Canyon, USA.
title_sort of travertine and time: otolith chemistry and microstructure detect provenance and demography of endangered humpback chub in grand canyon, usa.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2013-01-01
description We developed a geochemical atlas of the Colorado River in Grand Canyon and in its tributary, the Little Colorado River, and used it to identify provenance and habitat use by Federally Endangered humpback chub, Gila cypha. Carbon stable isotope ratios (δ(13)C) discriminate best between the two rivers, but fine scale analysis in otoliths requires rare, expensive instrumentation. We therefore correlated other tracers (SrSr, Ba, and Se in ratio to Ca) to δ(13)C that are easier to quantify in otoliths with other microchemical techniques. Although the Little Colorado River's water chemistry varies with major storm events, at base flow or near base flow (conditions occurring 84% of the time in our study) its chemistry differs sufficiently from the mainstem to discriminate one from the other. Additionally, when fish egress from the natal Little Colorado River to the mainstem, they encounter cold water which causes the otolith daily growth increments to decrease in size markedly. Combining otolith growth increment analysis and microchemistry permitted estimation of size and age at first egress; size at first birthday was also estimated. Emigrants < 1 year old averaged 51.2 ± 4.4 (SE) days and 35.5 ± 3.6 mm at egress; older fish that had recruited to the population averaged 100 ± 7.8 days old and 51.0 ± 2.2 mm at egress, suggesting that larger, older emigrants recruit better. Back-calculated size at age 1 was unimodal and large (78.2 ± 3.3 mm) in Little Colorado caught fish but was bimodally distributed in Colorado mainstem caught fish (49.9 ± 3.6 and 79 ± 4.9 mm) suggesting that humpback chub can also rear in the mainstem. The study demonstrates the coupled usage of the two rivers by this fish and highlights the need to consider both rivers when making management decisions for humpback chub recovery.
url http://europepmc.org/articles/PMC3865257?pdf=render
work_keys_str_mv AT karinelimburg oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
AT toddahayden oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
AT williamepine oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
AT michaeldyard oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
AT reinhardkozdon oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
AT johnwvalley oftravertineandtimeotolithchemistryandmicrostructuredetectprovenanceanddemographyofendangeredhumpbackchubingrandcanyonusa
_version_ 1725911938229075968