Progressive palaeoenvironmental change during the Late Barremian–Early Aptian as prelude to Oceanic Anoxic Event 1a: Evidence from the Gorgo a Cerbara section (Umbria-Marche basin, central Italy)

• Published in: Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2011-03, Vol.302 (3), p.396-406
• Main Authors: Stein, Melody, Föllmi, Karl B., Westermann, Stéphane, Godet, Alexis, Adatte, Thierry, Matera, Virginie, Fleitmann, Dominik, Berner, Zsolt
• Format: Article
• Language: English
• Subjects: Carbon and oxygen isotopes; Gorgo a Cerbara; Oceanic Anoxic Event 1a; Phosphorus; Redox-sensitive trace elements
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2011.01.025

During Oceanic Anoxic Event 1a (OAE 1a, 120 Ma; Li et al., 2008), organic carbon-rich layers were deposited in marine environments under anoxic conditions on a global scale. In this study, palaeoenvironmental conditions leading to this event are characterised by studying the Upper Barremian to the Lower Aptian succession of the Gorgo a Cerbara section (central Italy). For this, an integrated multi-proxy approach (δ 13C carb; δ 13C org; δ 18O; phosphorus; Total Organic Carbon, TOC; bulk-rock mineralogy, as well as redox-sensitive trace elements — RSTEs) has been applied. During the Late Barremian, thin organic-rich layers occur episodically, and associated C org:P tot ratios indicate the presence of intermittent dysoxic to anoxic conditions. Coarse correlations are observed between TOC, P and biogenic silica contents, indicating links between P availability, productivity, and TOC preservation. However, the corresponding δ 13C carb and δ 18O records remain quite stable, indicating that these brief periods of enhanced TOC preservation did not have sufficient impact on the marine carbon reservoir to deviate δ 13C records. Around the Barremian–Aptian boundary, TOC-enriched layers become more frequent. These layers correlate with negative excursions in the δ 13C carb and δ 13C org records, possibly due to a warming period as indicated by the δ 18O record. During the earliest Aptian, this warming trend is reverted into a cooling trend, which is then followed by an important warming step near the onset of Oceanic Anoxic Event 1a (OAE 1a). During this time period, organic-rich intervals occur, which are characterised by the progressive increase in RSTE. The warming step prior the onset of OAE 1a is associated with the well-known negative spike in δ 13C carb and δ 13C org records, an important peak in P accumulation, RSTE enrichments and C org:P tot ratios indicating the prevalence of anoxic conditions. The Selli Level itself may document a cooling phase. RSTE enrichments and C org:P tot ratios confirm the importance of anoxic conditions during OAE 1a at this site. The Gorgo a Cerbara section is interpreted to reflect the progressive impact of palaeoenvironmental change related to the formation of the Ontong-Java plate-basalt plateau, which started already around the Barremian–Aptian boundary and culminated into OAE 1a. ► New proxies for the Gorgo a Cerbara section (Italy). ► Progressive impact of palaeoenvironmental change during the Late Barremian. ► OAE 1a is the