The Toarcian Oceanic Anoxic Event in the Ionian Zone, Greece

• Published in: Palaeogeography, palaeoclimatology, palaeoecology Vol. 393; pp. 135 - 145
• Main Authors: Kafousia, N., Karakitsios, V., Mattioli, E., Kenjo, S., Jenkyns, H.C.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.01.2014; Elsevier
• Subjects: Calcareous nannofossils; Carbon isotopes; Chemostratigraphy; Earth Sciences; Jurassic; Sciences of the Universe; T-OAE; Calcareous nannofossils; Jurassic; Carbon isotopes; Chemostratigraphy; T-OAE
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2013.11.013

The Early Jurassic was characterized by a global disturbance of the carbon cycle known as the Toarcian Oceanic Anoxic Event (T-OAE). This event is recorded worldwide by a negative excursion in marine and terrestrial carbon-isotope ratios, typically interrupting an overarching positive trend attributed to large-scale burial of marine organic matter under oxygen-depleted conditions. The negative excursion is attributed to introduction of isotopically light carbon into the ocean–atmosphere system. Three sections from the Ionian Zone in Greece have been analysed in terms of biostratigraphy, Total Organic Carbon (TOC), CaCO3, δ13Ccarb, δ18Ocarb and δ13Corg. On the basis of bio- and chemostratigraphy, the age of Pliensbachian–Toarcian formations from the Ionian Zone in Greece has been refined and the geochemical signature of the T-OAE recognized. All sections illustrate the characteristic negative excursion in carbon isotopes from both carbonates and organic matter and, in only one locality, a positive excursion has also been recorded. The recognition of the T-OAE in this part of the Tethyan continental margin offers additional information on the global impact and amplitude of this important Jurassic palaeoceanographic event. •A high-resolution record of the T-OAE of the Ionian Zone has been established.•Nannofossil biostratigraphy allowed age assessment and correlation of sections.•The Pliensbachian/Toarcian boundary recognized in the Siniais Limestone formation.•The negative CIE occurs in NJT 6 Zone in all sections from Ionian Zone.•A positive CIE takes place in NJT 7 Zone in only one section (Petousi).