Geochemical Evidence of the Seasonality, Affinity and Pigmenation of Solenopora jurassica
Abstract
Solenopora jurassica is a fossil calcareous alga that functioned as an important reef-building organism during the Palaeozoic. It is of significant palaeobiological interest due to its distinctive but poorly understood pink and white banding. Though widely accepted as an alga there is still debate over its taxonomic affinity, with recent work arguing that it should be reclassified as a chaetetid sponge. The banding is thought to be seasonal, but there is no conclusive evidence for this. Other recent work has, however demonstrated the presence of a unique organic boron-containing pink/red pigment in the pink bands of S. jurassica. We present new geochemical evidence concerning the seasonality and pigmentation of S. jurassica. Seasonal growth cycles are demonstrated by X-ray radiography, which shows differences in calcite density, and by varying δ13C composition of the bands. Temperature variation in the bands is difficult to constrain accurately due to conflicting patterns arising from Mg/Ca molar ratios and δ18O data. Fluctuating chlorine levels indicate increased salinity in the white bands, when combined with the isotope data this suggests more suggestive of marine conditions during formation of the white band and a greater freshwater component (lower chlorinity) during pink band precipitation (δ18O). Increased photosynthesis is inferredmore »
- Authors:
-
- Univ. of Manchester (United Kingdom)
- SLAC National Accelerator Lab., Menlo Park, CA (United States)
- NERC Isotope Geosciences Facilities and Univ. of Nottingham, Nottingham (United Kingdom)
- Univ. of California, Davis, CA (United States)
- Publication Date:
- Research Org.:
- SLAC National Accelerator Laboratory (SLAC), Menlo Park, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1224051
- Grant/Contract Number:
- AC02-07CH11359
- Resource Type:
- Accepted Manuscript
- Journal Name:
- PLoS ONE
- Additional Journal Information:
- Journal Volume: 10; Journal Issue: 9; Journal ID: ISSN 1932-6203
- Publisher:
- Public Library of Science
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Barden, Holly E., Behnsen, Julia, Bergmann, Uwe, Leng, Melanie J., Manning, Phillip L., Withers, Philip J., Wogelius, Roy A., van Dongen, Bart E., and Silva, Lucas C. R. Geochemical Evidence of the Seasonality, Affinity and Pigmenation of Solenopora jurassica. United States: N. p., 2015.
Web. doi:10.1371/journal.pone.0138305.
Barden, Holly E., Behnsen, Julia, Bergmann, Uwe, Leng, Melanie J., Manning, Phillip L., Withers, Philip J., Wogelius, Roy A., van Dongen, Bart E., & Silva, Lucas C. R. Geochemical Evidence of the Seasonality, Affinity and Pigmenation of Solenopora jurassica. United States. https://doi.org/10.1371/journal.pone.0138305
Barden, Holly E., Behnsen, Julia, Bergmann, Uwe, Leng, Melanie J., Manning, Phillip L., Withers, Philip J., Wogelius, Roy A., van Dongen, Bart E., and Silva, Lucas C. R. Mon .
"Geochemical Evidence of the Seasonality, Affinity and Pigmenation of Solenopora jurassica". United States. https://doi.org/10.1371/journal.pone.0138305. https://www.osti.gov/servlets/purl/1224051.
@article{osti_1224051,
title = {Geochemical Evidence of the Seasonality, Affinity and Pigmenation of Solenopora jurassica},
author = {Barden, Holly E. and Behnsen, Julia and Bergmann, Uwe and Leng, Melanie J. and Manning, Phillip L. and Withers, Philip J. and Wogelius, Roy A. and van Dongen, Bart E. and Silva, Lucas C. R.},
abstractNote = {Solenopora jurassica is a fossil calcareous alga that functioned as an important reef-building organism during the Palaeozoic. It is of significant palaeobiological interest due to its distinctive but poorly understood pink and white banding. Though widely accepted as an alga there is still debate over its taxonomic affinity, with recent work arguing that it should be reclassified as a chaetetid sponge. The banding is thought to be seasonal, but there is no conclusive evidence for this. Other recent work has, however demonstrated the presence of a unique organic boron-containing pink/red pigment in the pink bands of S. jurassica. We present new geochemical evidence concerning the seasonality and pigmentation of S. jurassica. Seasonal growth cycles are demonstrated by X-ray radiography, which shows differences in calcite density, and by varying δ13C composition of the bands. Temperature variation in the bands is difficult to constrain accurately due to conflicting patterns arising from Mg/Ca molar ratios and δ18O data. Fluctuating chlorine levels indicate increased salinity in the white bands, when combined with the isotope data this suggests more suggestive of marine conditions during formation of the white band and a greater freshwater component (lower chlorinity) during pink band precipitation (δ18O). Increased photosynthesis is inferred within the pink bands in comparison to the white, based on δ13C. Pyrolysis Gas Chromatography Mass Spectrometry (Py-GCMS) and Fourier Transform Infrared Spectroscopy (FTIR) show the presence of tetramethyl pyrrole, protein moieties and carboxylic acid groups, suggestive of the presence of the red algal pigment phycoerythrin. This is consistent with the pink colour of S. jurassica. As phycoerythrin is only known to occur in algae and cyanobacteria, and no biomarker evidence of bacteria or sponges was detected we conclude S. jurassica is most likely an alga. Pigment analysis may be a reliable classification method for fossil algae.},
doi = {10.1371/journal.pone.0138305},
journal = {PLoS ONE},
number = 9,
volume = 10,
place = {United States},
year = {Mon Sep 14 00:00:00 EDT 2015},
month = {Mon Sep 14 00:00:00 EDT 2015}
}
Web of Science
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Works referencing / citing this record:
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