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Ecological and Environmental Change Research Group

IGNEX

Interglacials and glacials - natural experiments in biodiversity dynamics

ioannina-figure.jpg

Selected pollen spectra from Ioannina, NW Greece going back from the present day through the last glacial to the previous interglacial
Tree pollen diagram from the Ioannina basin in north-west Greece that covers the Holocene, the last glacial stage including the LGM with two early temperate interstadials, the last interglacial stage, and the penultimate glacial stage. It shows the local growth of deciduous Quercus (oak) during the LGM, presumably growing in the sort of mid-elevation refugium shown below in the picture from north-west Greece. Data from this site will be analysed in the IGNEX project. From Tzedakis et al. 2002 (Science 297: 2044-2047)
Photo:
Chronis Tzedakis et al.

IGNEX and its sister project IGNEX-eco will use the same datasets but very different numerical procedures and analytical techniques to address different aspects of long-term dynamics (IGNEX) and of ecosystem assembly and its relevance to restoration ecology (IGNEX-eco).

There are three major ecological hypotheses to explain plant community structure

  • extrinsic external environmental control where communities are structured primarily through plant responses to the environment, especially climate
  • intrinsic internal species interactions e.g. facilitation, mutualism, herbivory, and above all, competition
  • neutral dynamics, random processes and historical legacies

These hypotheses are not mutually exclusive and attempts are being made to unite them. Disentangling and assessing the relative roles of environment, interactions, and neutrality in plant community assembly, composition, and structure requires a historical dimension because, as Jeannine Cavender-Bares notes (in Stokstad 2009: Science) "you cannot understand the assembly process if you do not think about time" and as Steve Jackson and Jessica Blois (2015: PNAS) emphasise "a consensus is emerging that community properties cannot be understood without biogeographical and historical contexts". Long-tem palaeoecological data from detailed pollen analyses of continuous sequences covering 100,000 - 1,000,000 years provide the historical dimension.

During these time periods, Earth has experienced major climatic shifts from temperate interglacial stages (we live in the latest interglacial) to cool, often dry, glacial 'ice-age' stages. Due to advances in sediment coring and chronology and a huge amount of time-consuming pollen analysis, continuous records of pollen (and hence, by inference, vegetation) change through alternating interglacial and glacial stages from Greece, NE Russia, and Colombia are now available. Each of these records, plus sequences for three different interglacial stages in Denmark, provides a long-term ecological observatory. The changes from glacial to interglacial conditions are a series of 'natural experiments' on vegetation change and they can be used to test ecological hypotheses about the determinants of long-term community assembly, composition, and structure and of biodiversity dynamics (taxonomic, functional, phylogenetic) and turnover.

The IGNEX projects will use numerical methods to detect major recurring patterns of vegetation change, biodiversity, and turnover for each interglacial stage, for each glacial-interglacial pair, for all glacial stages, and for all interglacial stages. Six main hypotheses will be evaluated.

  1.  There are consistent patterns in taxonomic, functional, phylogenetic, and attribute diversity and compositional turnover between interglacials in a geographical area and within interglaciala of the same marine isotope stage (= age) in different areas - this will be a particular focus of IGNEX-eco.
  2. There is a complex dynamic of extrinsic environmental change, intrinsic species interactions, and ecological drift within a glacial and subsequent interglacial couplet.
  3. There are long-term ecological legacies where IG composition and biodiversity are contigent on the preceding glacial conditions.
  4. Different interglacials have different compositions. If so, are the assemblages, altough differing in composition, similar in taxonomic, functional, phylogenetic, and attribute diversity and do they show the same amout of compositional turnover? Are differences in IG composition and/or biodiversity explicable (in a statistical sense) in terms of environmental differences, particularly solar insolation?
  5. Different interglacials have assemblages and taxon combinations that do not occur today: no-analogue or 'novel' assemblages.
  6. There are consistent assembly patterns between different IGs, at least at the scale of functional traits or phylogenetic relationshps, if not at the scale of taxonomic identity - this will be a particular focus of IGNEX-eco.

Testing of these hypotheses is important in establishing 'baseline conditions' for restoration ecology, in predicting biotic responses to future environmental change, and in providing a factual basis for future conservation.

IGNEX and its sister project IGNEX-eco, involve 17 research colleagues and support staff

John Birks (PI), University of Bergen

Blas Benito, based at University of Bergen

Henry Hooghiemstra and Vladimir Torres, University of Amsterdam, The Netherlands

Ulrike Herzschuh, AWI Polar and Marine Research, Potsdam, Germany

Thomas Giesecke, Univesity of Göttingen, Germany

Anson Mackay and Chronis Tzedakis, University College London, UK

Petr Kunes, Charles University, Prague, Czech Republic

Bjørg Risebrobakken, Uni Research, Bergen

Vivian Felde, Hilary Birks, Alistair Seddon, Joe Chipperfield (now at NMBU), Linn Krüger, Cathy Jenks, University of Bergen

Cajo ter Braak, Wageningen, The Netherlands, will provide statistical advice and develop new procedures, particularly for palaeo-trait analysis.

Jacques-Louis de Beaulieu and Maurice Reille, Centre National de la Recherche Scientifique, Marseille, France

This project and IGNEX-eco are based on agreed data-sharing and collaboration. These two projects are a major international research effort that exploits the unique long continuous pollens equences as long-term natural experiments in biodiveristy dynamics, ecosystem assembly, vegetational dynamics, and applied palaeoecology.

 

If you are a STUDENT interested in participating in IGNEX or IGNEX-eco, for example through a Masters project, please contact John Birks.

 

IGNEX is a 3-year NFR-funded FRIMEDBIO project (249894) running from 1 August 2016 to 31 July 2020.