In quaternary paleontology, reconstructing late Pleistocene terrestrial ecosystems traditionally relied upon macrofossil remains—bones, teeth, and macrobotanical seeds—recovered from stratified cave deposits. However, such assemblages are intrinsically biased by taphonomic filters, including selective predator accumulation and differential preservation rates. The emergence of sediment ancient DNA (sDNA) analysis has bypassed these constraints by extracting trace organellar DNA directly from inorganic mineral matrices. Notably, while early sDNA protocols yielded inconsistent results due to DNA leaching across stratigraphic layers, recent methodological refinements using targeted hybridization capture have demonstrated that extracellular DNA binds tightly to clay minerals, specifically montmorillonite, preventing vertical migration even in humid karst environments. Contrary to initial assumptions that sDNA primarily records local micro-fauna brought in by owl pellets, comparative metagenomic profiling reveals that clay-bound mammalian DNA in cave fills predominantly originates from shed skin cells and metabolic waste carried by aeolian dust and meteoric water percolation, rather than biotic vectors. Consequently, sDNA profiles reflect regional mammalian community structure over multi-decadal accumulation windows, rather than immediate site-specific prey deposition.
Based on the passage, recent methodological refinements in sediment ancient DNA (sDNA) analysis established that vertical migration of extracellular DNA across stratigraphic layers is prevented primarily by which of the following mechanisms?
- The chemical binding of extracellular DNA to specific clay minerals such as montmorillonite.Cevap
- BThe physical trapping of organellar DNA within owl pellets deposited in unstratified cave fills.
- CThe elimination of aeolian dust and meteoric water percolation through targeted hybridization capture.
- DThe adherence of extracellular DNA to macrofossil seeds preserved within inorganic matrices.
- EThe complete suppression of meteoric water flow within humid karst cave environments.