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MEPS 754:17-33 (2025)  -  DOI: https://doi.org/10.3354/meps14773

Foraminiferal assemblages and organic matter relationships in a coastal lagoon on the arid coast of the Southeast Pacific

Alexa Narciso-Mezones1, Lander Merma-Mora1, Kathy Córdova-Rodríguez1,2, Carol Rocca1, Matthieu Carré1,3, Pedro E. Romero4, Rodolfo Salas1, Alexander Pérez1, Edgar Cruz-Acevedo1,5, Diana Ochoa1,6, Jorge Cardich1,*

1Laboratorios de Investigación y Desarrollo (LID)-Facultad de Ciencias e Ingeniería, Centro de Investigación para el Desarrollo Integral y Sostenible (CIDIS), Universidad Peruana Cayetano Heredia, 15102 Lima, Perú
2Facultad de Ciencias Veterinarias y Biológicas, Universidad Científica del Sur, 15067 Lima, Perú
3Laboratoire d’Océanographie et du Climat: Expérimentations et Approches Numériques (CNRS, IRD, MNHN, Sorbonne Université), 75005 Paris, France
4Facultad de Ciencias Biológicas, Universidad Nacional Mayor de San Marcos, 15081 Lima, Perú
5Departamento de Ciencias Exactas y Desarrollo Humano, Facultad de Ciencias Biológicas, Universidad Autónoma de Nuevo León, 66450 San Nicolás de los Garza, México
6Geology Department, Salamanca University, 37008 Salamanca, Spain
*Corresponding author:

ABSTRACT: The Southeast Pacific arid zone, encompassing Peruvian and Chilean coastal deserts, features several wetlands that are influenced by upwelling waters and provide critical ecosystem services. Despite the significance of wetlands such as the coastal lagoon Poza La Arenilla (PLA) in Lima, Peru, their proximity to urban areas exposes them to eutrophication. This, in turn, presents considerable challenges for conservation efforts. Effective conservation strategies demand a comprehensive assessment of trophic conditions, achieved here by studying living and dead benthic foraminifera assemblages. These microorganisms serve as bioindicators for organic sources and enrichment. We explored their relationships with hydrological factors (dissolved oxygen, temperature, salinity) and sedimentary parameters (total organic matter, carbon, nitrogen, stable isotopes) in the PLA. Our results show that foraminifera distribution is influenced by organic matter (OM) from marine phytoplankton/algae and bacterial sources. Foraminifera were dominated by hyaline and soft-walled species, and 4 distinct foraminiferal assemblages were identified. Psammophaga sp1 prevailed in areas with abundant OM, while Bathysiphon sp. was associated with less organic conditions in sandy sediments. Additionally, Quinqueloculina seminulum, Buliminella elegantissima, Ammonia confertitesta, and Bathysiphon sp. were frequent and abundant species in the PLA. Dead assemblages showed a 2-fold increase in species richness compared to living foraminifera, indicating seasonal species turnover. Our study evidenced the importance of the whole diversity of foraminifera for environmental and/or ecological assessments, as groups of soft-walled and agglutinated foraminifera comprise potential bioindicators for eutrophication.


KEY WORDS: Coastal lagoons · Foraminifera · Soft-walled · Organic matter · Bioindicator


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Cite this article as: Narciso-Mezones A, Merma-Mora L, Córdova-Rodríguez K, Rocca C and others (2025) Foraminiferal assemblages and organic matter relationships in a coastal lagoon on the arid coast of the Southeast Pacific. Mar Ecol Prog Ser 754:17-33. https://doi.org/10.3354/meps14773

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