Evidence map›Paper›PMID 32084252›Full record

ArticlePloS one2020

Aquatic community structure as sentinel of recent environmental changes unraveled from lake sedimentary records from the Atacama Desert, Chile.

Adriana Aránguiz-Acuña, José A Luque, Héctor Pizarro, Mauricio Cerda, Inger Heine-Fuster, Jorge Valdés, Emma Fernández-Galego, Volker Wennrich

Open access · goldAbstract read
In one paragraph

Article in PloS one, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
0.8field-weighted citation impact, top 29% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed, 14 citations in OpenAlex.

  1. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

8 authors at 4 institutions in 3 countries.

Adriana Aránguiz-AcuñaCentro de Investigación Tecnológica del Agua en el Desierto (CEITSAZA-UCN), Antofagasta, Chile.ORCID 0000-0002-9409-1147
José A LuqueDepartamento de Ciencias Geológicas, Universidad Católica del Norte, Antofagasta, Chile.
Héctor PizarroDepartamento de Ciencias Geológicas, Universidad Católica del Norte, Antofagasta, Chile.
Mauricio CerdaLaboratório de Biogeoquimica de Ambientes Aquáticos Universidade Federal Fluminense (PPBMAC-UFF), Rio de Janeiro, Brazil.
Inger Heine-FusterCentro de Investigación Tecnológica del Agua en el Desierto (CEITSAZA-UCN), Antofagasta, Chile.
Jorge ValdésInstituto Alexander von Humboldt, Universidad de Antofagasta, Antofagasta, Chile.
Emma Fernández-GalegoInstitute of Geology & Mineralogy, University of Cologne, Cologne, Germany.
Volker WennrichInstitute of Geology & Mineralogy, University of Cologne, Cologne, Germany.ORCID 0000-0003-3617-1963
Universidad de Antofagasta · CLUniversidad Católica del Norte · CLUniversity of Cologne · DEUniversidade Federal do Rio de Janeiro · BR

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Atacama Desert (21-26°S) is currently one of the driest places on Earth and metal(loid)s are of special concern for this region, which hosts the largest-known porphyry copper deposits produced in Chile. Evidence of past environmental conditions is commonly preserved in natural archives, such as lacustrine sediments. Sediment records obtained from Inca Coya Lake (22°20'S-68°35'W, 2534 m.a.s.l.), a small lake located in the Atacama Desert, reflected the evolution of regional mining activity during the 20th century and sedimentation associated with decadal climate variability. We studied the aquatic community structure changes recorded in sediment records from Inca Coya Lake. By analysis of magnetic properties (susceptibility, hysteresis curves and Curie temperatures), grain size and geochemical composition of the sediments, we identified environmental periods and changes in the community of benthic and planktonic organisms (diatoms and diapausing egg bank). We identified three detrital episodes that we interpret as dry/wet phases during the last 90 years associated with the increase of flash flood events promoting hypoxia oscillations; anthropogenic (mining activity) signals were also identified. Invertebrate community structure (primary consumers) reflected the metal exposure, measured as changes in assemblage composition through species turnover. Diatom community composition was best associated with variables related to wetter/drier alternation and consequent changes in oxygen availability. Bioindicators analyzed (diatoms, diapausing egg bank and invertebrate community) demonstrated to be excellent indicators of the bioavailability of compounds in the aquatic ecosystem of Inca Coya Lake, allowing the environmental impact assessment of the water resources due to flash floods and mining activity in the driest desert of the world.

Indexed as

EcosystemAnimalsAquatic OrganismsChileDesert ClimateEnvironmental MonitoringGeologic SedimentsLakesMagneticsMetalsMetals

Identifiers

PMID32084252
PMCPMC7034912
OpenAlexW3007211106

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.