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  • CRC1211 - Earth – Evolution at the dry limit

Project D4

Project

Project ended after 2nd Phase

Reconstructing changes of water sources and availability by combined lipid biomarker and online stable isotope and radiocarbon analysis

Research areas: Geochronology, Organic Geochemistry, Method Development

Principal investigators: Prof. Dr. Janet Rethemeyer, Dr. Markus Schiffer

 

Project Info: Phase 2

The hyperarid soils of the Atacama Desert frequently served as model systems for tracing life under extremely dry conditions. Water availability is the main controlling factor determining the presence of life. The abundance and distribution of plants is largely dependent on fog moisture and irregular rainfalls associated with the El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) climate phenomena and follows latitudinal and elevational gradients. Traces of plant and microbial life preserved in the desert soils, which were analysed during the 1st funding period, showed a strong dependency on water availability increasing in abundance and diversity from the hyperarid core of the desert to wetter sites at higher elevations. Fog, related to the marine Stratocumulus cloud, is the ultimate water source in coastal areas. Its spatial and temporal variability is, however, difficult to constrain. We thus evaluated the utility of nitrogen (δ15N) and hydrogen (δ2H) isotopic signatures in plant tissues and leaf waxes, respectively, of living and fossil Tillandsia plants as proxies for present and past fog water availability. Our results showed that plant tissue δ15N values correlate significantly with precipitation, total cloud cover as well as cloud height along a 300 km coastal transect in northern Chile. In addition, δ15N and δ2H results of fossil Tillandsia plant layers excavated from sand dunes indicated a distinct dry episode during late Medieval times known as a period of extreme long-lasting droughts related to a major ENSO anomaly, thus holding great potential for reconstruction changes in fog moisture at high temporal resolution using new archives collected during the 2nd phase of the CRC.

The main focus of D04 during the 2nd funding period will be on three aspects including:

  1. the development of ultra-small-scale AMS 14C analysis (1-20 µg C) and its application for solving dating problems in different CRC projects
  2. the reconstruction of past changes in water supply in fossil Tillandsia dunes and other suitable archives and its effect on the stable isotopic composition (δ2H, δ13C, δ15N, δ34S) in living Tillandsia
  3. the identification and age determination of traces of life in desert soils along moisture and depth gradients based on lipid biomarker and radiocarbon analyses.

 

Fieldwork 2017: unique Tillandsia landbeckii ecosystems located in the Coastal Cordillera depend solely on fog moisture. We use the information preserved in relict Tillandsia plants buried in sand dunes to reconstruct past climate change (photos: A. Jaeschke).

 

 

 



Contact

  Speaker:
Prof. Dr. Tony Reimann
Institute of Geography | University of Cologne
Zülpicher Str. 45 | 50674 Cologne
+49 (0)221 470-1724 | t.reimann@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. Christine Heim
Institute of Geology and Mineralogy | University of Cologne

Zülpicher Str. 49b | 50674 Cologne
+49 (0)221 470-90341 | christine.heim@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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