Benthic response to the strong Silurian climatic fluctuations—implications from Gotland (Sweden)

• Published in: Facies Vol. 70; no. 4
• Main Authors: Claussen, Anna Lene, Munnecke, Axel
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01-10-2024; Springer Nature B.V
• Subjects: Arid climates; Benthic communities; Benthos; Biogeosciences; Carbon isotopes; Carbonate rocks; Carbonates; Chemical analysis; Climate; Climate change; Climate models; Coastal processes; Coastal zone; Corals; Earth and Environmental Science; Earth Sciences; Ecology; Geochemistry; Gypsum; Humid climates; Isotope ratios; Ocean models; Original Article; Paleontology; Phanerozoic; Phosphorus; Phosphorus cycle; Reefs; Seawater; Sedimentology; Silurian; Water analysis; Gotland (island); Reef development; Isotope excursion; Phosphorus cycle; Bryostromatolites; Bryozoa
• ISSN: 0172-9179; 1612-4820
• DOI: 10.1007/s10347-024-00686-x

Climatically the Silurian was a most unstable period, as it is shows several strong δ
13
C excursions, with the Lau excursion being the strongest short-lived positive δ
13
C excursion of the entire Phanerozoic. The causes of these excursions remain a topic of debate. In order to determine how benthic communities responded to these climatic perturbations, a microfacies analysis of carbonate rocks from the Silurian period (Late Telychian to the uppermost Ludfordian) of Gotland was conducted. The development of reefs was significantly enhanced during periods characterized by carbon isotope excursions, compared to time intervals without. In periods of elevated δ
13
C values (≥ 3 ‰) the abundance of bryozoans and microbes increases, and in some areas, they form reefs (bryostromatolites), while corals and stromatoporoids were the main reef builders in periods of lower isotope ratios (0–3 ‰). Furthermore, a significant increase of phosphatic components, gypsum pseudomorphs and the microproblematicum
Palaeomicrocodium
is observed in times of increased isotope ratios. A model is proposed that explains the changes in the benthic communities over time. It is based on previously published models and explains the geochemical processes from coastal areas to the open ocean. Changes are assumed from a humid climate in times without isotope excursions to an arid climate in times of isotope excursions. It emphasizes processes that may have led to the strong δ
13
C shifts during the Silurian period, and includes the phosphorus cycle in sea water as an important factor in the development of the benthic communities.