Serpulid microbialitic bioherms from the upper Sarmatian (Middle Miocene) of the central Paratethys Sea (NW Hungary) – witnesses of a microbial sea

• Published in: Biogeosciences Vol. 20; no. 23; pp. 4775 - 4794
• Main Authors: Harzhauser, Mathias, Mandic, Oleg, Piller, Werner E.
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 04-12-2023; Copernicus Publications
• Subjects: Accretion; Alkalinity; Arid climates; Bioherms; Biological activity; Concrete; Coral reefs; Dental cement; Deposition; Endangered & extinct species; Environmental factors; Environmental parameters; Growth; Marine environment; Marine fishes; Microbial activity; Microorganisms; Miocene; Mollusks; Neogene; Sand & gravel; Sediment; Sediments; Tubes; Hungary; Austria
• ISSN: 1726-4189; 1726-4170; 1726-4189
• DOI: 10.5194/bg-20-4775-2023

We present previously unknown stacked bowl-shaped bioherms reaching a size of 45 cm in diameter and 40 cm in height from weakly solidified peloidal sand from the upper Sarmatian of the Paratethys Sea. The bioherms were mostly embedded in sediment, and the “growth stages” reflect a reaction on sediment accretion and sinking into the soft sediment. The bioherms are spirorbid–microclot–acicular cement boundstones with densely packed Janua tubes surrounded by microclots and acicular cement solidifying the bioherm. The surrounding sediment is a thrombolite made of peloids and polylobate particles (mesoclots) which are solidified synsedimentarily by micrite cement and dog-tooth cement in a later stage. The shape of the bioherms reflects a series of growth stages with an initial stage (“start-up stage”) followed by a more massive “keep-up stage” which grades into a structure with a collar-like outer rim and a central protrusion and finally by a termination of growth (“give-up stage”). The setting was a shallow subtidal environment with normal marine or elevated saline, probably oligotrophic, conditions with an elevated alkalinity. The stacked bowl-shaped microbialites are a unique feature that has so far been undescribed. Modern and Neogene microbialite occurrences are not direct analogues to the described structures, but the marine examples, like in The Bahamas, Shark Bay and the Persian Gulf, offer insight into their microbial composition and environmental parameters. The microbialites and the surrounding sediment document a predominance of microbial activity in the shallow marine environments of the Paratethys Sea during the late Middle Miocene, which was characterized by a warm, arid climate.