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Project Introduction B3 - Protist Evolution at the Dry Limit

Project Introduction B3 - Protist Evolution at the Dry Limit

In Project B3, we aim to investigate the co-evolution of gregarine protists (microscopic organisms living in the gut of insects), with their hosts (endemic darkling beetles) and the co-evolution of free-living protists with the geological evolution of the landscape.

We were able to find protistan life even at very hostile places. Within groups of well described organisms, we were able to find and describe new families, genera and species especially adapted to hyperarid conditions. One of this species is extremely well adapted to the prevailing conditions Enibas tolerabilis which belongs to a completely new evolutionary lineage of choanoflagellates, the sister group of all metazoans.

The Atacama Desert offers the unique opportunity to study the evolution and speciation of protists in the context of geological evolutionary processes. Protists are eukaryotic organisms (cells containing a nucleus) that are not animals or plants. In Project B3, we aim to investigate the co-evolution of gregarine protists, which are parasites with a size of up to about half a millimeter, with their hosts (endemic darkling beetles). Furthermore, we focus on the speciation of aquatic protists in salars with extreme chemical and physical properties, which demands a specific adaptation of protists. These investigations in close cooperation with geologists can serve as a model to study evolutionary processes and substitution rates [changes in the sequence of genes] in protists in general. A third research focus is the diversity of protists associated to endemic plants. As there are barely any fossil records of unicellular eukaryotes, Project B3 is intended to determine evolutionary processes in this hostile environment and to get an idea of the speed of evolutionary processes in unicellular eukaryotes of various phylogenetic lineages.

“Even in hostile places like the salars with a high content of salts and toxins like Arsenic, exposed to extremely high UV radiation, we were able to find protist life. And not only life, our first data indicate that Chile's Atacama Desert may act as a center of species radiation.“
– Prof. Dr. Hartmut Arndt

The high number of protist species, which we were able to isolate and cultivate up to now, allows a deeper insight into evolutionary processes driven by the harsh environment in the Atacama Desert. We were able to analyze species from several evolutionary lineages within the tree of life, gaining even a deeper insight into the origin of life and evolution at the dry limit. Our first results correspond well with geological datings and are the first step to add valuable data to substitution and mutation rates in protists. Having now these species in culture will allow us to perform experiments on their ecological functions and to their analysis on a molecular level to understand the underlying mechanisms.

 

Publication

Contact

Prof. Dr. Hartmut Arndt
Phone: +49 (0) 221 470-3100
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Dr. Frank Nitsche
Phone: +49 (0) 221 470-3100
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Bärbel Jendral
Phone: +49 (0) 221 470-3100
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Project

Project Introduction D4 - Trace organic compounds

Project Introduction D4 - Trace organic compounds

Tracing water availability, organic carbon sources, and life at the dry limit using radiocarbon analysis

Our project is about reconstructing changes in water availability and its effect on organic carbon sources in desert soils. We use the information encoded in the distribution and isotopic composition of molecular fossils, i.e. remnants of plant and microbial life, for the identification of microbial communities as well as of climate variability past and present. A major part of our work is dedicated to technical and methodological developments for radiocarbon dating of very small samples (i.e. extremely low organic carbon content).

The most challenging aspect is to extract traces of plant and microbial life and to get age information by radiocarbon dating from soils located in the hyperarid core of the desert that exposes very low organic carbon contents. For instance, we need to extract about 5 kg of soil to obtain few micrograms of plant-derived organic matter. Therefore, major analytical developments are required to enable the analysis of these samples.

“Exploring life at the dry limit is a very fascinating topic and doing fieldwork in the hyperarid core of the Atacama felt like being on Mars. The project gives us the unique opportunity to study distinct plant and microbial communities which developed a very specific life style to grow and survive at such extreme climatic conditions. We were surprised by the good preservation of organic compounds originating from plant remains, which enabled us to analyze their isotopic composition for paleoclimate reconstruction.”
– Janet Rethemeyer

 

Publication:

  • Rethemeyer, J., Gierga, M., Heinze, S., Stolz, A., Wotte, A., Wischhöfer, P., Berg, S., Melchert, J.O., Dewald, A., 2019. Current sample preparation and analytical capabilities of the radiocarbon laboratory at CologneAMS. Radiocarbon, doi.org/10.1017/RDC.2019.16.
  • Stolz, A., Dewald, A., Heinze, S.., Altenkirch, R., Hackenberg, G., Herba, S., Müller-Gatermann, C., Schiffer, M., Zitzer, G., Wotte, A., Rethemeyer, J., Dunai, T., 2019. Improvements in the measurement of small 14CO2 samples at CologneAMS. Nuclear Instr. and Methods in Physics Res. B 439, 70-75.
  • Stolz, A., Dewald, A., Altenkirch, R., Herb, S., Heinze, S., Schier, M., Feuerstein, K., Müller-Gatermann, C., Wotte, A., Rethemeyer, J., Dunai, T., 2017. Radiocarbon measurement of small gaseous samples at CologneAMS. Nuclear Inst. and Methods in Physics Res. B 406, 283-286.

Contact
Prof. Dr. Janet Rethemeyer

Phone: +49 (0)221 470-7317
E-Mail: This email address is being protected from spambots. You need JavaScript enabled to view it.

 


Project

Project Introduction D5 – OSL Dating

Constraining the Pleistocene environmental history of the Atacama: Extending the age range of luminescence dating

The D05 project uses optically stimulated luminescence (OSL) dating, a technique that informs about the timing of sediment deposition, to provide chronological constraints for landscape and climate evolution of the Atacama Desert. By applying OSL dating, temporal patterns for geomorphologic and climatic changes deduced from sediment records such as alluvial fans, clay pans or hillslope deposits can be established. This includes the application of conventional OSL dating approaches as well as the development of new techniques that enable to target sediments which can as yet not be dated.

Due to the high age of the Atacama Desert many sediment records exceed the age range of conventional OSL dating. Therefore, a special focus of project D05 is the development of new techniques that can extend the conventional age range of OSL dating. The innovative technique investigated in this project is optically stimulated luminescence  dating using violet stimulation (VSL), which will allow to date much older sediments than can be achieved using the techniques available until now.

We are among the first to further advance and apply this specific dating technique (VSL dating). It gives information on geomorphologic structures and climatic events in the Atacama Desert that so far could not be dated by any other approach.

 

Contact

Prof. Dr. Helmut Brückner
Phone +49 (0)221 470-1724
E-Mail This email address is being protected from spambots. You need JavaScript enabled to view it.

 

Since sunlight effects the luminescence signal, any form of light exposure must be avoided during sample collection in the field. In order to avoid sunlight exposure of the sediments from the 50 m drill core, samples from core barrels were collected in a completely lightproof tent next to the drill location using head lights equipped with red light (which does not affect the luminescence signal). Extremely hot temperatures in this tent due to strong insolation and missing ventilation were challenging.

Pressen Eulychnia TBoehnert TB011954 1 350px Photo: D. Brill

 

Pressen Eulychnia TBoehnert TB011954 1 350pxPhoto: D. Brill

 

Pressen Eulychnia TBoehnert TB011954 1 350px Photo: Georgina King

 

Pressen Eulychnia TBoehnert TB011954 1 350pxPhoto: Georgina King


Project

Project Introduction A3  - Aeolian transport

Project Introduction A3 - Aeolian transport

Statistical-dynamical modelling of aeolian processes in the Atacama Desert over geological time scales and their implications to life at the dry limit.

 

IMG 1029 1 350px MODIS true-color image of the dust plume over the coast of northern Chile on July 8, 2016
Source:
https://www.earthobservatory.nasa.gov

In project A03 we study weather types over the Subtropical Southeast Pacific. The focus of our research of these weather types in the Atacama Desert is their impact on climate and aeolian transport which plays a major role in shaping the surface. We study both present-day and paleo-climate conditions, going back from thousands to millions of years. To do this, a regional climate model (Weather Research and Forecasting Model, WRF) is used to simulate climate and surface processes on high spatial resolution to obtain detailed data on the conditions in the Atacama Desert. The overall goal of the project is to better understand the processes important for the geomorphological and biological evolution in this extremely dry region of the Earth, to test various hypotheses and provide paleo-climate and -environment data to other projects of the CRC.

“This is what I find particularly interesting. The CRC brings together researchers from different disciplines to study the extreme environment of the Atacama Desert.”
– Dr. Mark Reyers

For the first time, we have developed an objective classification of weather types for the Atacama region, which can be applied to global paleo-climate simulations and is useful for many other applications, such as the assessment of water resources and renewable energy resources. Further, a set of long-term regional climate simulations for the Atacama Desert under the present-day and paleo-climate conditions has been  established and will be made available for the research community at large.

 

 Publication:

  • Reyers M, Hamidi M, Shao Y (2019): Synoptic analysis and simulation of an unusual dust event over the Atacama Desert. Atmospheric Science Letters. DOI:10.1002/asl.899 (https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/asl.899)
  • Reyers M, Shao Y (2019): Cutoff lows off the coast of the Atacama Desert under present day conditions and in the Last Glacial Maximum. Global and Planetary Change 181 (2019) 102983

Contact

Prof. Dr. Yaping Shao
Phone: +49 (0)221 470-3688
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Dr. Mark Reyers
Scientist in A3
Phone: +49 (0)221 470-7302
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Project



Contact

  Speaker:
Prof. Dr. Tibor J. Dunai
Institute of Geology and Mineralogy | University of Cologne
Zülpicher Str. 49b | 50674 Cologne
+49 (0)221 470-3229 | tdunai@uni-koeln.de
   
  Managing Director:
Christian Tiede
Institute of Geology and Mineralogy | University of Cologne

Zülpicher Str. 49b | 50674 Cologne
+49 (0)221 470-89833 | christian.tiede@uni-koeln.de

 _

  Co-Speaker:
Prof. Dr. Martin Melles
Institute of Geology and Mineralogy | University of Cologne

Zülpicher Str. 49a | 50674 Cologne
+49 (0)221 470-2262 | mmelles@uni-koeln.de
   
  Scientific Coordinator:
Dr. Benedikt Ritter
Institute of Geology and Mineralogy | University of Cologne

Zülpicher Str. 49b | 50674 Cologne
+49 (0)221 470-89868 | benedikt.ritter@uni-koeln.de

 _

  Co-Speaker:
Prof. Dr. Dietmar Quandt
Nees Institute for Biodiversity of Plants | University of Bonn

Meckenheimer Allee 170 | 53115 Bonn
+49 (0)228 73-3315 | quandt@uni-bonn.de
   
  Webmaster:
Tim Schlüter
Institute of Geography | University of Cologne

Otto-Fischer-Str. 4 | 50674 Cologne
+49 (0)221 470-3735 | webmaster@sfb1211.de
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