Data Preparation#
The Atacama soil microbiome dataset [D1] contains:
\(N = 50\) samples from Atacama Desert soil
\(p = 13\) microbial taxa (ASVs)
\(q = 5\) environmental covariates: pH, elevation, temperature, humidity, and vegetation
Data Overview describes the dataset in more detail.
Transforming the counts#
Microbiome counts represent relative abundances constrained to sum to a constant. Transform them before estimating a covariance.
# Transform compositional data using mCLR transformation
qiime gglasso transform-features \
--p-transformation mclr \
--p-add-metadata False \
--p-scale-metadata False \
--i-table data/atacama-counts.qza \
--i-taxonomy data/classification.qza \
--m-sample-metadata-file data/selected-atacama-sample-metadata.tsv \
--o-transformed-table data/atacama-table-mclr.qza
The modified centred log-ratio moves the table into an unconstrained space, handles zeros
without adding pseudo-counts, and preserves the relative information between taxa. For the
standard centred log-ratio instead, pass --p-transformation clr.
Building the input correlation#
qiime gglasso calculate-covariance \
--p-method scaled \
--i-table data/atacama-table-mclr.qza \
--o-covariance-matrix data/atacama-table-corr.qza
A scaled covariance is the Pearson correlation. For the covariance itself, pass
--p-method unscaled.
The input to the graphical lasso problem must be a positive semi-definite matrix.