“…The density values estimated in this study were eight times above those reported by Soltwedel (2000) for tropical areas, which, according to Coull (1999), are in the order of 1,000 ind/10 cm 2 in soft marine sediments. This is evidenced when comparing the densities obtained in depths of the Venezuelan territorial sea, in which the density of meiobenthos was between 13-153 ind/10 cm 2 (Woods & Tietjen, 1985), the central zone of the Great Barrier Reef in Australia (26 m deep) with 220-1,010 ind/10 cm 2 (Hansen et al 1987), southeastern Costa Rica (5 m deep) with 99-575 ind/10 cm 2 (Guzmán et al 1987), Rocks Atoll in northeast Brazil (2.5 m deep) with 278-4,165 ind/10 cm 2 (Netto et al 2003), Bay Lagoon in Jamaica (<10 m deep) with 327.7-5,518.9 ind/10 cm 2 (Edwards, 2009), Cienfuegos Bay in Cuba (9 m deep) with 780.02 ± 772 ind/10 cm 2 (Armenteros et al 2009), intertidal zones in Suriname and French Guiana (<1 m deep) with 1,760-4,400 ind/10 cm 2 (Dupuy et al 2015), and tropical beaches in Brazil (<6 m deep) with 288-2,553 ind/10 cm 2 (Baia & Venekey, 2019). These differences could be the result of different depths, temperatures, and other environmental conditions.…”