Variability of macrofauna distribution along a dissipative log-spiral sandy beach in Rio de Janeiro, Southeastern Brazil

Carlos A.M. Barboza; Tatiana Cabrini; Gustavo Mattos; Viviane Skinner; Ricardo Cardoso

doi:10.3989/scimar.04467.03A

Autores/as

Carlos A.M. Barboza Departamento de Ecologia e Recursos Marinhos, Universidade Federal do Estado do Rio de Janeiro (UNIRIO) - Núcleo em Ecologia e Desenvolvimento Sócio-Ambiental de Macaé, Universidade Federal do Rio de Janeiro https://orcid.org/0000-0002-5922-5410
Tatiana Cabrini Departamento de Ecologia e Recursos Marinhos, Universidade Federal do Estado do Rio de Janeiro (UNIRIO) - Programa de Pós-graduação em Ecologia, Universidade Federal do Rio de Janeiro (UFRJ) https://orcid.org/0000-0003-2006-7328
Gustavo Mattos Programa de Pós-graduação em Ecologia, Universidade Federal do Rio de Janeiro (UFRJ) https://orcid.org/0000-0003-3677-4190
Viviane Skinner Departamento de Ecologia e Recursos Marinhos, Universidade Federal do Estado do Rio de Janeiro (UNIRIO) https://orcid.org/0000-0003-1343-4214
Ricardo Cardoso Departamento de Ecologia e Recursos Marinhos, Universidade Federal do Estado do Rio de Janeiro (UNIRIO) https://orcid.org/0000-0002-8692-0283

DOI:

https://doi.org/10.3989/scimar.04467.03A

Palabras clave:

facies de macrofauna, playas curvadas, meso-escala, intermareal, morfodinámica, gradientes físicos

Resumen

Las playas en espiral muestran gradientes físicos definidos a lo largo de su recorrido. En este trabajo se investiga la relación entre la distribución en la estructura de comunidades de la macrofauna de una playa y sus gradientes físicos mediante el estudio de 10 transectos. El análisis de componentes principales reveló un claro gradiente físico a lo largo de la playa. El análisis de redundancia mostró que el extremo protegido se caracterizó con tamaños de grano menor, mayor contenido de materia orgánica y uma mayor densidad de anélidos poliquetos. El extremo expuesto se caracterizó por arena gruesa, bajo contenido de materia orgánica y una alta densidad de crustáceos. El mejor ajuste para explicar el número de individuos en una muestra se relacionó con el tamaño del grano de arena y la pendiente de la playa. La variabilidad del poliqueto Scolelepis squamata se explicó mejor en base al tamaño de grano, la pendiente y la selección de su sedimento. Por su parte, el mejor modelo para explicar la variabilidad del cirolánido Excirolana armata solo incluyó la selección del sedimento. El gradiente físico en la textura del sedimento y la pendiente de la playa explicó más de la tercera parte de la variabilidad en la estructura comunitaria. A su vez, las variables físicas también se correlacionaron con la distribución de especies individuales de la macrofauna. El gradiente físico en las playas en espiral puede explicar la variabilidad de su macrofauna, incluso a mesoescala y en condiciones disipativas.

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