Abstract

Living benthic foraminifera (>63 µm) were studied to characterize the continental slope of the Potiguar Basin (SW Atlantic). Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characterization. It was also estimated if and which changes occur when the subsurface is added. Sampling stations were distributed in five transects in four isobaths (150, 400, 1000, and 2000 m). Sediment samples were fixed with 4% buffered formaldehyde and stained with Bengal rose. Were recorded 396 species in the surface layer, 228 in the subsurface, and 449 in integrating both layers. This study did not include tubular agglutinated species. The assemblages from 150 m isobath indicated the upper slope, from 400 m indicated the middle slope and the ones from the 2000 m indicated the lower slope. The surface layer’s assemblage at 1000 m isobath was more similar to the middle slope; in contrast, its subsurface layer’s assemblage had more similarity with the lower slope. Rarefaction curves, Permanova, and NMDS routines indicated a high resemblance between surface and integrated layers. Therefore, the first two centimeters were sufficient to characterize this region based on living benthic foraminifera.

Highlights

  • The widespread use of these organisms promoted the establishment of guidelines for environmental monitoring of marine ecosystems and a protocol with standardized methods for soft-bottom benthic foraminiferal monitoring studies [6]

  • Microhabitats may change seasonally, and the species or genera can be found in different sediment layers according to favorable conditions or due to their development [8]

  • The highest sand content was observed at MT54 and MT53 (94.21% and 91.48%, respectively)

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Summary

Introduction

The study of Foraminifera is an important tool for environmental quality assessment, as they are abundant and collectible, have short life cycles, are sensitive to physical and chemical changes in the environment, and change the composition of their assemblages and their distribution in regions impacted by pollution [1,2,3,4,5]. Benthic foraminifers do not live only at the sediment-water interface but can be found several centimeters deep in marine sediments. These microhabitats have a combination of physical, chemical, and biological characteristics. The species that inhabit superficial layers may differ from those inhabiting deeper layers forming assemblages with different faunal compositions [7]. Microhabitats may change seasonally, and the species or genera can be found in different sediment layers according to favorable conditions or due to their development [8]

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