Stable isotope evidence from archived fish scales indicates carbon cycle changes over the four-decade history of the Rimov Reservoir (Czechia).

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F21%3A00542650" target="_blank" >RIV/60077344:_____/21:00542650 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.1016/j.scitotenv.2020.142550" target="_blank" >https://doi.org/10.1016/j.scitotenv.2020.142550</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.scitotenv.2020.142550" target="_blank" >10.1016/j.scitotenv.2020.142550</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Stable isotope evidence from archived fish scales indicates carbon cycle changes over the four-decade history of the Rimov Reservoir (Czechia).

Popis výsledku v původním jazyce

Using archived fish scale samples together with long-term monitoring data, this study investigates the potential of fish scales to record historical changes in the aquatic environment. We analysed stable carbon (delta C-13) and nitrogen (delta N-15) isotopes in the scales of two planktivorous cyprinid species collected from the meso-eutrophic Rimov Reservoir, Czechia, over its entire four-decade history (1979-2016). The delta C-13 of the fish scales varied greatly throughout the reservoir history. The lowest delta C-13 values were observed immediately after the reservoir was filled in 1979, indicating that fish production at that time was likely partially supported by C-13-depleted CO2 released from the inundated soil. During the 1980s, due to the high levels of phytoplankton production stimulated by high phosphorus inputs from the catchment, the delta C-13 values substantially increased. However, since 1990, the delta C-13 values have generally decreased, reflecting a gradual reduction in reservoir primary production caused by the decreasing input of phosphorus and increasing input of dissolved organic carbon from the catchment. The delta C-13 of fish scales was also used to reconstruct the CO2 concentration of the surface water. The reconstructed CO2 varied significantly during the four-decade history, but it was always below the air-equilibrium concentration, suggesting that the surface water of the reservoir has consistently absorbed atmospheric carbon. The fish-scale delta N-15 values remained relatively stable, while slightly increasing within three years after impoundment, likely because the nitrogen supply was high throughout the studied period. Our study contributes to the growing body of literature demonstrating that stable isotope analysis of archived biological samples is a promising approach for understanding historical trends in the biogeochemistry of aquatic environments. In particular, our results highlight the potential of delta C-13 in archived fish scales in reconstructing carbon cycle changes and evaluating human impacts on aquatic ecosystems.

Název v anglickém jazyce

Stable isotope evidence from archived fish scales indicates carbon cycle changes over the four-decade history of the Rimov Reservoir (Czechia).

Popis výsledku anglicky

Using archived fish scale samples together with long-term monitoring data, this study investigates the potential of fish scales to record historical changes in the aquatic environment. We analysed stable carbon (delta C-13) and nitrogen (delta N-15) isotopes in the scales of two planktivorous cyprinid species collected from the meso-eutrophic Rimov Reservoir, Czechia, over its entire four-decade history (1979-2016). The delta C-13 of the fish scales varied greatly throughout the reservoir history. The lowest delta C-13 values were observed immediately after the reservoir was filled in 1979, indicating that fish production at that time was likely partially supported by C-13-depleted CO2 released from the inundated soil. During the 1980s, due to the high levels of phytoplankton production stimulated by high phosphorus inputs from the catchment, the delta C-13 values substantially increased. However, since 1990, the delta C-13 values have generally decreased, reflecting a gradual reduction in reservoir primary production caused by the decreasing input of phosphorus and increasing input of dissolved organic carbon from the catchment. The delta C-13 of fish scales was also used to reconstruct the CO2 concentration of the surface water. The reconstructed CO2 varied significantly during the four-decade history, but it was always below the air-equilibrium concentration, suggesting that the surface water of the reservoir has consistently absorbed atmospheric carbon. The fish-scale delta N-15 values remained relatively stable, while slightly increasing within three years after impoundment, likely because the nitrogen supply was high throughout the studied period. Our study contributes to the growing body of literature demonstrating that stable isotope analysis of archived biological samples is a promising approach for understanding historical trends in the biogeochemistry of aquatic environments. In particular, our results highlight the potential of delta C-13 in archived fish scales in reconstructing carbon cycle changes and evaluating human impacts on aquatic ecosystems.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10618 - Ecology

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2021

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Science of the Total Environment

ISSN

0048-9697

e-ISSN

1879-1026

Svazek periodika

755

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

10

Strana od-do

142550

Kód UT WoS článku

000600786700021

EID výsledku v databázi Scopus

2-s2.0-85092236673