Buracas: Novel and unusual sinkhole-like features in the Abrolhos Bank

• We have mapped 36 sinkhole-like features along the Abrolhos Bank.
• They occur in a consolidated carbonate substrate at various depths.
• They present no relation between their diameter, depth, and distance from the coast.
• Their origin could be related to either typical sinkhole formation or to a Holocene growth pattern.

Novel and unusual sinkhole-like features are described for the Abrolhos Bank continental shelf, eastern Brazil, based on geophysical and geological assessments. These unusual structures are large cup-shaped depressions similar to sink/blueholes (10–75 m in diameter, 8–39 m in height), occurring in a consolidated carbonate substrate in the mid and outer shelf. A total of 36 such features, locally named buracas, were found between 41 and 161 km off the coast and between 24 and 65 m depth (the bottom of these features may be as deep as 93 m). The buracas’ walls are mainly composed of encrusting coralline algae. Radiocarbon dating has provided ages of 5400±90 yr Cal BP, 8630±90 yr Cal BP and 39,200±400 yr BP. Besides providing a comprehensive description of these novel structures within the mesophotic zone, the potential mechanisms by which these sinkhole-like structures originated are discussed here, as well as the possible active mechanisms impeding their filling with sediments and biogenic material. We hypothesize that their origin could be related to either typical sinkhole formation during subaerial exposure or to a partially Holocene growth pattern influenced by antecedent morphology and gas/fluid escaping due to organic matter decomposition. The buracas are relevant not only because they comprise outstanding novel features, but also because they are relevant targets for marine conservation, as they enhance productivity and aggregate biomass in a region under growing fishing pressure.