3rd Polar Marine Diatom Taxonomy and Ecology Workshop


Sydney, Australia, 4-8 July 2011

Diatoms are key organisms at the base of high-latitude communities throughout the late Paleogene and Neogene. Their fossil remains serve as a fundamental basis for age determination and paleoenvironmental reconstruction, and are key indicators of marine paleotemperatures, presence/absence of sea ice, and the advance and retreat of ice sheets and shelves - all important geological data that can feed into ice-sheet and climate models.

The workshop was attended by 27 diatomists from 11 countries and was hosted by Leanne Armand at the Department of Biological Sciences, Macquarie University. International participation (especially at the graduate student and post-doctoral level) was instrumental in the transfer of sound taxonomic skills and the exchange of knowledge relative to modern and fossil diatom records of the polar regions. These skills are key to understanding the ecologic and micropaleontologic records of the poles. This meeting was timely for the hands-on transfer of results from the successful Antarctic Drilling (ANDRILL) project (Ross Sea), several recent Integrated Ocean Drilling Program (IODP) Legs (Wilkes Land, Campbell Plateau, and Bering Sea), and a suite of polar marine-based projects hosted at the national level (such as the US NSF-sponsored Larsen Ice Shelf System – Antarctica LARISSA project).

The two primary goals of the workshop were: (1) to provide the international community of polar diatom research with an opportunity to exchange data, discuss taxonomic issues toward standardization of terminology and identifications, and to explore new techniques and approaches, and (2) to allow students to receive training and advice from leaders in the field.

Mornings were devoted to taxonomic work at the microscope and based on participants’ slide sets that highlighted particular genera and species. These sessions focused on identification of key extant and extinct paleoenvironmental indicators in both the Antarctic and Arctic regions, understanding the environmental implications of morphological variability within single species, and recognition of important biostratigraphic markers ranging back to the Eocene (ca. 56-34 Ma). In the afternoons, advances in the field were discussed. These included the application of biomarker and stable isotopic studies to biosiliceous sediments, the role of dissolution in altering the diatom paleo-record, and lessons learned through studies of modern phytoplankton.

In addition, two keynote speakers shared their expert knowledge with participants: Diana Krawczyk (University of Szczecin, Poland) spoke about her paleoclimatic research off West Greenland, addressing the local implications of ocean-climate forcing and the expression of late Holocene climatic events (such as the Little Ice Age and the Medieval Climate Anomaly) in the marine diatom sedimentary record. Simon Wright (Australian Antarctic Division and Antarctic Climate and Ecosystems Cooperative Research Centre) provided a larger scale framework for diatom studies through his work on the responses of Southern Ocean phytoplankton to climate change.

One of the intended objectives of this workshop was to bring together students and early career researchers with the intention that the weeklong conversations and discussions would lead to future research collaborations. The next Polar Marine Diatom workshop is planned for 2013 and will be hosted by Jenny Pike (Cardiff University, UK). Previous workshop accomplishments are reported by Armand (2006), Assmy (2008) and Leventer et al. (2007).

In addition to PAGES, the workshop was also supported by the ARC Research Network for Earth System Science, the Australian Marine Geoscience Office, Geoscience Australia, the Australian Biological Resources Study, Macquarie University, ATA Scientific and ANDRILL.


Figure 1: Comparison of marine phytoplankton species-richness curve indicated by Falkowski et al. (2004) with chronologic ranges of cetacean families worldwide by Uhen (2007), and sea-level change. Global deep-sea oxygen record and paleo-temperature change are by Zachos et al. (2001) and the presence data of sea ice and ice sheets were compiled by St. John (2008) and Stickley et al. (2009). The Atlantic Chaetoceros Explosion (ACE) event occurred across the E/O boundary in the North Atlantic, and is characterized by resting spore diversification that occurred as a consequence of upwelling activation following changes in thermohaline circulation through global cooling in early Oligocene. Pacific Chaetoceros Explosion events-1 and -2 (PACE-1 and PACE-2) are characterized by relatively higher occurrences of iron input following the Himalayan uplift and aridification at 8.5 Ma and ca. 2.5 Ma in the North Pacific regions. From Itsuki Suto, Nagoya University, Japan.

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