@misc{10481/112221,
year = {2026},
month = {3},
url = {https://hdl.handle.net/10481/112221},
abstract = {Bioherms are common in the pre-evaporitic Messinian in Neogene basins in SE Spain. Coral 
bioherms reported to date in the region have been interpreted as shallow-water reefs based on 
coral morphology (stick-like Porites and Tarbellastraea domes) and surrounding sediments. 
However, at the western margin of the Almería–Níjar Basin, coral bioherms grew in relatively 
deep waters with low turbidity on the eastern shelf of the upland precursor to the Sierra de 
Gádor. Bioherms occur in the lower part of a reef unit, in some cases growing directly on the 
erosion surface separating this unit from the underlying older Miocene rocks. They are formed 
mainly by Porites, with minor Tarbellastraea, encrusted by foraminifera, coralline algae and 
microbialite. The thickness of bioherms ranges from less than 1 m to about 20 m in the largest 
bioherm. Mesophotic conditions can be inferred from direct palaeodepth measurements at the 
outcrop, showing that bioherms started to develop at several tens of metres water depth. The 
dominance of thin, laminar, contorted Porites colonies with few finger-like projections is also 
indicative of low light levels. Facies laterally equivalent to the bioherms—namely algal/bivalve 
wackestone to packstone, rhodolith rudstone rich in coralline algae of the order Hapalidiales, and 
Halimeda floatstone to rudstone—are all characteristic of relatively deep waters in the Mediterranean Neogene. The low siliciclastic content of bioherms and surrounding deposits 
(<8%) suggests that low light conditions in which bioherms grew were primarily due to water 
depth. The Almería bioherms are the first record of Upper Miocene blue mesophotic reefs in the 
world.},
organization = {Junta de Andalucia - (RMN189) (RMN190)},
publisher = {Elsevier},
keywords = {Porites},
keywords = {Coral morphology},
keywords = {Halimeda beds},
title = {Blue mesophotic coral bioherms in the pre-evaporitic Messinian of the western Mediterranean (Almería–Níjar Basin, SE Spain)},
doi = {10.1016/ j.palaeo.2026.113724},
author = {Sola, Fernando and Braga Alarcón, Juan Carlos},
}