hasData_Center_Short_Name |
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hasDataset_Online_Resource |
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hasProject_Long_Name |
- High-resolution CONTINENTal paleoclimate record in Lake Baikal
- Ice Expedition 2001
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hasDataset_Release_Date |
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hasDataset_Title |
- Depth profiles of marker pigments from Bacillariophyceae plus Chrysophyceae (A), Chlorophyta (B), cyanobacterial picoplankton (C), Eustigmatophyceae, and Cryptophyta (D).
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hasEntry_ID |
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hasKeyword |
- Alloxanthin influx
- Chlorophyll b influx
- Chlorophyll c influx
- Violaxanthin influx
- Zeaxanthin influx
- diatoxanthin influx
- fucoxanthin influx
- lutein influx
- pheophytin b influx
- ß-carotene influx
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hasReference |
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10.1016/j.gloplacha.2004.11.004
http://dx.doi.org/10.1016/j.gloplacha.2004.11.004
S. Fietz, M. Sturm and A. Nicklisch, Flux of lipophilic photosynthetic pigments to the surface sediments of Lake Baikal, Glob. Planet. Change 46 (2005), pp. 2944.
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hasSummary |
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The traps were deployed for about 16 months. The respective regression equations and its coefficients of determination (r2) are reported in Table 5.In the 40-m trap, fucoxanthin was the dominant carotenoid (Table 1 and Fig. 3). Other pigments of Bacillariophyceae plus Chrysophyceae (chlorophyll c, diadinoxanthin, and diatoxanthin) as well as the cyanobacterial zeaxanthin also showed high sedimentation rates, whereas the chlorophyte chlorophyll b and lutein, as well as the cryptophyte alloxanthin, sedimented only in low amounts (Table 1 and Fig. 3). Abbreviations: Chlchlorophyll, Fucofucoxanthin, Zeazeaxanthin, β-carβ-carotene, Alloalloxan
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