Interacción sedimentaria del polvo sahariano, y los flujos biogénicos y litogénicos en la cuenca oceánica de Canarias
DOI:
https://doi.org/10.3989/scimar.04877.19APalabras clave:
flujos litogénicos, flujos biogénicos, flujos POC, TEP, análisis de imagen, polvo sahariano, cuenca oceánica de CanariasResumen
En la actualidad los eventos de polvo Sahariano son la fuente principal de partículas litogénicas en la cuenca oceánica de Canarias. Con el objetivo de cuantificar su entrada y la interacción con los flujos biogénicos, se instaló una trampa de sedimento a la deriva, a 150 m de profundidad, 50 km al norte de la costa de Gran Canaria (Islas Canarias). Las partículas litogénicas detectadas fueron de illita, calcita, hematites, cuarzo, barita y caolinita. El material biogénico estaba compuesto por quitina, partículas de exopolímeros transparentes (TEP) y carbonatos procedentes de foraminíferos y conchas de gasterópodos. La media del flujo de polvo sahariano sobre la superficie oceánica fue aproximadamente 5±4 mg m-2 dia-1. Las medias de flujos litogénico, carbonato y quitina respectivamente fueron 0.8±0.6 mg m-2 dia–1, 6.0±7.4 mg m–2 dia-1 y 154±386 mg m-2 dia-1. Durante el muestreo se registró un intenso evento de polvo sahariano seguido, a los tres días, de picos en los flujos litogénicos y biogénicos en la trampa de sedimento a 150 m de profundidad. La velocidad teórica de sedimentación de las partículas litogénicas asociadas a los eventos de polvo sahariano a 150 m de profundidad calculada fue de vStokes=275 m dia-1, siendo la velocidad de sedimentación experimental obtenida tras el análisis de los flujos fue de 50 m dia-1. El comportamiento de los procesos de sedimentación asociados al POC, el flujo biogénico y el flujo litogénico observados en este estudio podría contribuir a modelos más realistas de la bomba biológica de carbono en los océanos.
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