Resilience of an aquatic macrophyte to an anthropogenically induced environmental stressor in a Ramsar wetland of southern Chile.

Environmental changes Iron loads in plants Spatial occurrence of aquatic macrophytes Wetland

Journal

Ambio
ISSN: 1654-7209
Titre abrégé: Ambio
Pays: Sweden
ID NLM: 0364220

Informations de publication

Date de publication:
Mar 2019
Historique:
received: 22 09 2017
accepted: 16 06 2018
revised: 11 01 2018
pubmed: 5 7 2018
medline: 12 10 2019
entrez: 5 7 2018
Statut: ppublish

Résumé

In mid-2004, anthropogenically induced changes in water quality of the Río Cruces wetland, a Ramsar site located in southern Chile (ca. 40°S), enhanced the resuspension of iron-enriched sediments, which were subsequently deposited over the most abundant aquatic macrophyte of the wetland (Egeria densa Planch. 1849). This event triggered the formation of brownish, necrotic patches and increased iron contents in the leaves and stems of E. densa, which contributed to a significant demise of the plant within the wetland. In this study, we estimate the recovery time as a proxy for resilience of this macrophyte at organismal and population levels. Macro- and micro-optical characteristics, as well as iron contents in tissues of E. densa, were documented in four time windows (2004, 2008, 2012, and 2014). In addition, the size of the macrophyte population and its spatial occurrence were monitored from 2008 to 2016 across 36 study sites within the wetland. Our results suggest necrotic patches and high iron contents in E. densa persisted at least until 2008. After 2013, a significant increase in the spatial occurrence of E. densa was observed within the wetland, reaching full recovery of the population during 2015. The health of plant tissues and iron contents in leaves and stems showed recovery period close to 4 years, while the recovery of the spatial occurrence of E. densa took approximately 9 years. While the monitoring of plant health was not performed on a strict annual basis, the recovery rates estimated here are slower than those described for other macrophytes. This finding might reflect the long-lasting effects of the disturbance from 2004 and the interaction with biotic processes, such as foraging by waterbirds recolonizing the Río Cruces wetland. These results show that full recovery of E. densa was achieved through a cascade of effects starting with abiotic factors (water quality) and passing through physiological and individual levels, to finally reach the population level. A key aspect of this response is the invasive nature of the macrophyte, which likely contributed to its recovery as a consequence of improved water quality. Less successful macrophyte species in other systems may not reach the specific population recovery, and become subdominant species instead, or even be eradicated from the wetland either as the result of herbivory or due to competition with other macrophytes.

Identifiants

pubmed: 29971664
doi: 10.1007/s13280-018-1071-6
pii: 10.1007/s13280-018-1071-6
pmc: PMC6374225
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

304-312

Subventions

Organisme : CONAMA
ID : 1210-1203/2004

Références

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pubmed: 26433547
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pubmed: 18074900

Auteurs

Eduardo Jaramillo (E)

Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile. edojaramillo@gmail.com.

Cristian Duarte (C)

Departamento de Ecología y Biodiversidad, Facultad de Ecología y Recursos Naturales, Universidad Andres Bello, Santiago, Chile.

Fabio A Labra (FA)

Centro de Investigación e Innovación, para el Cambio Climático, Facultad de Ciencias, Universidad Santo Tomás, Santiago, Chile.

Nelson A Lagos (NA)

Centro de Investigación e Innovación, para el Cambio Climático, Facultad de Ciencias, Universidad Santo Tomás, Santiago, Chile.

Bruno Peruzzo (B)

Instituto de Anatomía, Histología y Patología, Facultad de Medicina, Universidad Austral de Chile, Valdivia, Chile.

Ricardo Silva (R)

Instituto de Anatomía, Histología y Patología, Facultad de Medicina, Universidad Austral de Chile, Valdivia, Chile.

Carlos Velasquez (C)

Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile.

Mario Manzano (M)

Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile.

Daniel Melnick (D)

Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile.

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