Tracing Aridity: Sedimentary Preservation of Scytonemin from Microbiotic Desert Soil Crusts
Deserts are a critical end-member in biome reconstructions used to help constrain our understanding of paleoclimatology. Yet given the lower fossilization potential for desert plants and animals, direct paleontological evidence of climate change is much less abundant from arid environments than from other terrestrial ecosystems. However, following the model of wind-blown pollen, potentially continuous sedimentary records can be derived from small eolian particles carrying molecular biomarkers. We posit that one such molecule is scytonemin, a pigment that is produced by cyanobacteria in desert microbiotic soil crusts to protect against UV exposure. We have recently published a mid-Holocene record of sedimentary scytonemin from the Black Sea, and stable isotope analysis supports a desert microbiotic soil source for these molecules. Furthermore, this record coincided with 7-methylheptadecane, which is also enriched in desert microbiotic soil cyanobacteria. We recently conducted a pilot study of scytonemin in Great Salt Lake sediments and found a similar signal recorded by a scytonemin degradation product, suggesting that scytonemin is a representative tracer of cyanobacteria in desert microbioitic soil crusts. Thus, we hypothesize that scytonemin is an aridity indicator, with increased accumulation when deserts expand and cyanobacteria-dominated microbiotic soil crusts become more prevalent.We propose developing scytonemin and 7-methylheptadecane as molecular biomarkers to reconstruct records of past aridity in the late Quaternary and deeper into the Phanerozoic.
We plan to address four overarching questions:
- Does scytonemin degradation yield molecular fragments that are chemically recognizable and analytically tractable in ancient geological samples?
- What is the physiological relationship between scytonemin and 7-methylheptadecane production in desert microbiotic soil cyanobacteria?
- Do scytonemin and 7-methylheptadecane distributions in the Great Salt Lake and Gulf of California reflect changes in aridity since the Last Glacial Maximum?