Climate Change in the Southern Ocean During the Middle Eocene to Early Oligocene: A Palynological Perspective

• Main Author: Storkey, Claire Andrea
• Format: Thesis
• Language: unknown
• Published: 2013
• Subjects: Earth Sciences not elsewhere classified; Dinocysts; Eocene/ Oligocene; Southern Ocean; School: School of Geography; Environment and Earth Sciences; 049999 Earth Sciences not elsewhere classified; Marsden: 260112 Palaeontology; Marsden: 260113 Palynology; Degree Discipline: Geology; Degree Level: Doctoral; Degree Name: Doctor of Philosophy; Antarctic; The Antarctic; Weddell Sea; Kerguelen; Weddell; Marsden; Campbell Plateau; Georgia Rise; Northeast Georgia Rise; Antarc*
• Online Access: https://doi.org/10.26686/wgtn.17003965.v1; https://figshare.com/articles/thesis/Climate_Change_in_the_Southern_Ocean_During_the_Middle_Eocene_to_Early_Oligocene_A_Palynological_Perspective/17003965

The Antarctic and Southern Ocean is an area that was greatly affected by climatic changes during the Middle Eocene to Early Oligocene (E/O). This study aims to document climate-induced changes of the marine palynomorphs (mostly dinoflagellate cysts) by developing a Circum-Antarctic biozonation, and establishing the distribution and effects of cooling on the palynomorph assemblages and the palaeoenvironment. Samples were obtained from four sites by the Ocean Drilling Program (ODP) and Deep Sea Drilling Project (DSDP) and the palynological content was analyzed. These sites were selected as they may record effects of circulation changes and cooling trends, reflecting climate changes. ODP site 696B, was inner neritic and located in the South Orkney microcontinent, Weddell Sea. The other three sites were pelagic with ODP 699A located on the Northeast Georgia Rise, Falklands, ODP 748B located in the Western part of the Raggart Basin, Kerguelen Plateau and DSDP 277 located in Cathedral Depression on the Southern Campbell Plateau. From this analysis a comprehensive record of the local climatic transitions was ascertained, utilising assemblages of fossil organic-walled dinoflagellate cysts (dinocysts), acritarchs, prasinophyte algae, microforaminiferal linings, scoledonts and terrestrial material. The establishment of a standard nannofossil biostratigraphy provided a temporal framework of the marine palynomorphs in each site. Key dinocyst datums recognised as first or last occurrences that correlated reliably between sites, were compared with the nannofossil zones of each site. The purpose was to provide a Middle Eocene/Early Oligocene dinocyst biostratigraphy that temporally constrains the assemblages. Six primary datums and two secondary datums resulted, which lead to the recognition of four biozones and established a new biozonation in the Southern Ocean. The zones identified various dinocyst events, giving an indication of their probable palaeoenvironments. The Circum-Antarctic distribution pattern of palynomorph ...