DEP was performed on electrodes with different gap size values.
Appropriate effective sample size values (ESS > 200) for each parameter in the model were checked in Tracer v1.636.
Convergence was assessed through examination of effective sample size values (>1000) and posterior probability histograms for smooth, single-peak distributions.
Chain convergence was determined using Tracer v1.5 (http://tree.bio.ed.ac.uk/software/tracer/) to ensure sufficiently large effective sampling size values (>200).
All other units are ignored and the PSF map is treated as having logical pixel size values.
The monolayer sorption and average pore size values were estimated by applying BET and GAB models.
The CLC de novo algorithm (CLC bio) was used for assembling raw reads into contigs using different k-mer size values ranging from 32 to 50.
The sortable silt grain size values are highest from 9100 to 5000 years BP, suggesting a period of enhanced current circulation at the seabed.
The effective sample size values were all >800, and the topology of the tree was identical to the topology of the maximum likelihood tree inferred from the concatenation of the 1000 randomly selected orthologs using RAxML v.8.2.410 (not shown).
These grain size values are different from the crystallite size values obtained from the XRD analysis.
The optimal GOP size values are 64 and 128.
