Heavy metal movement through insect food chains in pristine thermal springs of Yellowstone National Park

Author:

Adams Braymond1,Bowley John2,Rohwer Monica3,Oberg Erik4,Willemssens Kelly3,Wintersteen Wendy1,Peterson Robert K.D.2,Higley Leon G.3

Affiliation:

1. Department of Plant Pathology, Entomology, and Microbiology, Iowa State University, Ames, IA, United States of America

2. Department of Land Resources & Environmental Sciences, Montana State University, Bozeman, MT, United States of America

3. School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE, United States of America

4. Yellowstone National Park, Gardner, MT, United States of America

Abstract

Yellowstone National Park thermal features regularly discharge various heavy metals and metalloids. These metals are taken up by microorganisms that often form mats in thermal springs. These microbial mats also serve as food sources for invertebrate assemblages. To examine how heavy metals move through insect food webs associated with hot springs, two sites were selected for this study. Dragon-Beowulf Hot Springs, acid-sulfate chloride springs, have a pH of 2.9, water temperatures above 70 °C, and populations of thermophilic bacterial, archaeal, and algal mats. Rabbit Creek Hot Springs, alkaline springs, have a pH of up to 9, some water temperatures in excess of 60 °C, and are populated with thermophilic and phototrophic bacterial mats. Mats in both hydrothermal systems form the trophic base and support active metal transfer to terrestrial food chains. In both types of springs, invertebrates bioaccumulated heavy metals including chromium, manganese, cobalt, nickel, copper, cadmium, mercury, tin and lead, and the metalloids arsenic, selenium, and antimony resulting from consuming the algal and bacterial mat biomass. At least two orders of magnitude increase in concentrations were observed in the ephydrid shore fly Paracoenia turbida, as compared to the mats for all metals except antimony, mercury, and lead. The highest bioaccumulation factor (BAF) of 729 was observed for chromium. At the other end of the food web, the invertebrate apex predator, Cicindelidia haemorrhagica, had at least a 10-fold BAF for all metals at some location-year combinations, except with antimony. Of other taxa, high BAFs were observed with zinc for Nebria sp. (2180) and for Salda littoralis (1080). This accumulation, occurring between primary producer and primary consumer trophic levels at both springs, is biomagnified through the trophic web. These observations suggest trace metals enter the geothermal food web through the microbial mat community and are then transferred through the food chain. Also, while bioaccumulation of arsenic is uncommon, we observed five instances of increases near or exceeding 10-fold: Odontomyia sp. larvae (13.6), P. turbida (34.8), C. haemorrhagica (9.7), Rhagovelia distincta (16.3), and Ambrysus mormon (42.8).

Funder

Therion, LLC, Brian Fiske, the Robert Allen Wright Endowment of Iowa State University, Montana State University, and the Montana Agricultural Experiment Station, and the University of Nebraska-Lincoln

Publisher

PeerJ

Reference48 articles.

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2. Arsenic and mercury distribution in an aquatic food chain: importance of femtoplankton and picoplankton filtration fractions;Alowaifeer;Environmental Toxicology and Chemistry,2023

3. Geothermal elements in lichens of Yellowstone National Park, USA;Bennett;Environmental and Experimental Botany,1999

4. QSAR models for the prediction of dietary biomagnification factor in fish;Bertato;Toxics,2023

5. Thermoregulatory adaptations of the wetsalts tiger beetle, Cicindelidia haemorrhagica, in Yellowstone National Park;Bowley;MS Thesis,2021

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