This vignette documents the data format used in
PLNmodel by PLN
and its variants. It also
shows how to create an object in the proper format for further analyses
from (i) tabular data, (ii) biom-class objects and (iii) phyloseq-class
objects.
We illustrate the format using trichoptera data set, a full description of which can be found in the corresponding vignette.
The trichoptera data set is a list made of two data frames:
Abundance
(hereafter referred to as the counts)
and Covariate
(hereafter the covariates).
## List of 2
## $ Abundance:'data.frame': 49 obs. of 17 variables:
## $ Covariate:'data.frame': 49 obs. of 7 variables:
The covariates include, among others, the wind, pressure and humidity.
## [1] "Temperature" "Wind" "Pressure" "Humidity"
## [5] "Cloudiness" "Precipitation" "Group"
In the PLN framework, we model the counts from the covariates, let’s say wind and pressure, using a Poisson Log-Normal model. Most models in R use the so-called formula interface and it would thus be natural to write something like
Unfortunately and unlike many generalized linear models, the response in PLN is intrinsically multivariate: it has 17 dimensions in our example. The left hand side (LHS) must encode a multivariate response across multiple samples, using a 2D-array (e.g. a matrix or a data frame).
We must therefore prepare a data structure where
Abundance
refers to a count matrix whereas
Wind
and Pressure
refer to vectors
before feeding it to PLN
. That’s the purpose of
prepare_data
.
trichoptera2 <- prepare_data(counts = trichoptera$Abundance,
covariates = trichoptera$Covariate)
str(trichoptera2)
## 'data.frame': 49 obs. of 9 variables:
## $ Abundance : num [1:49, 1:17] 0 0 0 0 0 0 0 0 0 0 ...
## ..- attr(*, "dimnames")=List of 2
## .. ..$ : chr [1:49] "1" "2" "3" "4" ...
## .. ..$ : chr [1:17] "Che" "Hyc" "Hym" "Hys" ...
## $ Temperature : num 18.7 19.8 22 23 22.5 23.9 15 17.2 15.4 14.1 ...
## $ Wind : num -2.3 -2.7 -0.7 2.3 2.3 -2 -4.7 -1 -2.7 -3.7 ...
## $ Pressure : num 998 1000 997 991 990 ...
## $ Humidity : num 60 63 73 71 62 64 93 84 88 75 ...
## $ Cloudiness : num 19 0 6 81 50 50 100 19 69 6 ...
## $ Precipitation: num 0 0 0 0 0 0 1.6 0 1.6 0 ...
## $ Group : Factor w/ 12 levels "1","2","3","4",..: 1 1 1 1 1 1 1 1 1 1 ...
## $ Offset : num 29 13 38 192 79 18 8 34 12 4 ...
If you look carefully, you can notice a few difference between
trichoptera
and trichoptera2
:
list
whereas the second is a
data.frame
1;Abundance
is a matrix-column of
trichoptera2
that you can extract using the usual functions
[
and [[
to retrieve the count matrix;trichoptera2
has an additional Offset
column (more on that later).It is common practice when modeling count data to introduce an offset term to control for different sampling efforts, exposures, baselines, etc. The proper way to compute sample-specific offsets in still debated and may vary depending on the field. There are nevertheless a few popular methods:
Each of these offset be computed from a counts matrix using the
compute_offset
function and changing its
offset
argument:
## same as compute_offset(trichoptera$Abundance, offset = "TSS")
compute_offset(trichoptera$Abundance)
## 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16
## 29 13 38 192 79 18 8 34 12 4 4 3 49 33 600 172
## 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32
## 58 51 56 127 35 13 17 3 27 40 44 8 9 1599 2980 88
## 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48
## 135 327 66 90 63 15 14 20 70 53 95 43 62 149 16 31
## 49
## 86
In this particular example, the counts are too sparse and sophisticated offset methods all fail (numeric output hidden)
## Warning in offset_function(counts, ...): Some samples only have 1 positive
## values. Can't compute quantiles and fall back to TSS normalization
## Warning in offset_function(counts, ...): Because of high sparsity, some samples
## have null or infinite offset.
We can mitigate this problem for the RLE offset by adding pseudocounts to the counts although doing so has its own drawbacks.
## 1 2 3 4 5 6 7 8
## 0.9186270 0.8349121 0.8570257 0.9186270 0.9186270 0.8349121 0.8192245 0.8570257
## 9 10 11 12 13 14 15 16
## 0.7322797 0.7322797 0.6321923 0.6321923 0.9240361 0.9186270 1.3788037 0.9240361
## 17 18 19 20 21 22 23 24
## 0.9186270 0.9240361 0.9240361 1.7140514 0.8908577 0.8570257 0.8349121 0.6321923
## 25 26 27 28 29 30 31 32
## 0.9240361 0.9240361 0.9186270 0.8570257 0.8349121 2.7721084 3.2934218 0.9584503
## 33 34 35 36 37 38 39 40
## 1.0406547 0.9584503 0.9584503 0.9186270 0.9584503 0.8908577 0.8349121 0.7322797
## 41 42 43 44 45 46 47 48
## 0.9240361 0.9240361 0.9584503 0.9584503 1.2643846 1.7140514 0.8233555 0.8908577
## 49
## 0.9186270
A better solution consists in using only positive counts to compute the offsets:
## 1 2 3 4 5 6 7 8
## 0.5631099 0.9462046 0.8299806 0.9462046 0.6460415 0.5756774 0.6308031 0.4947789
## 9 10 11 12 13 14 15 16
## 0.7988730 0.3574190 0.2207270 0.1260525 0.8051707 0.7289732 1.5591914 1.1850090
## 17 18 19 20 21 22 23 24
## 0.6389431 1.0000000 1.4606879 1.8224330 0.8403498 0.3942114 0.4058586 0.1997183
## 25 26 27 28 29 30 31 32
## 0.6286560 0.5631099 0.8777257 0.3440303 0.2504662 2.7086423 2.5800932 1.4584997
## 33 34 35 36 37 38 39 40
## 2.6050843 4.5898981 1.2185072 1.2616062 0.8823673 0.6250713 0.3950030 0.5631099
## 41 42 43 44 45 46 47 48
## 1.4511384 1.0000000 0.9462046 1.0882448 1.0000000 1.0631099 0.4621924 0.7900060
## 49
## 1.0672361
Finally, we can use wrench to compute the offsets:
## [1] 0.41269451 0.17385897 0.31925785 0.70682391 0.44749382 0.20676142
## [7] 0.10226641 0.21204241 0.09228293 0.03919178 0.03946910 0.02295077
## [13] 24.18096281 1.54038084 3.95187144 0.80172207 10.52136472 4.55854738
## [19] 0.46968859 51.88528943 0.32803605 0.14764973 4.13635353 0.03152826
## [25] 1.63626578 0.53769290 0.38482355 0.62689594 0.08030685 83.87692476
## [31] 33.40810265 0.75508731 1.05809625 1.18385013 0.58657751 0.43005272
## [37] 4.79925224 0.18381986 0.16078594 0.18490773 4.25999137 5.46689591
## [43] 0.60139850 7.56594658 9.89766712 33.73727074 0.74264459 29.13747796
## [49] 47.12017975
Note TSS is the only methods that produces offset on
the same scale as the counts, all others produces offsets that are
(hopefully) proportional to library sizes but on a different
scale. To force the offsets to be on the same scale as the counts for
all methods, you can use the option scale = "count"
.
## 1 2 3 4 5 6
## 17.2788462 7.2791915 13.3668057 29.5935647 18.7358369 8.6567635
## 7 8 9 10 11 12
## 4.2817277 8.8778701 3.8637358 1.6408958 1.6525069 0.9609112
## 13 14 15 16 17 18
## 1012.4174950 64.4932346 165.4584151 33.5667961 440.5123899 190.8589478
## 19 20 21 22 23 24
## 19.6650957 2172.3524890 13.7343345 6.1818537 173.1823794 1.3200369
## 25 26 27 28 29 30
## 68.5077809 22.5123254 16.1119346 26.2471113 3.3623170 3511.7901098
## 31 32 33 34 35 36
## 1398.7427987 31.6142749 44.3007651 49.5658750 24.5590443 18.0056062
## 37 38 39 40 41 42
## 200.9368679 7.6962380 6.7318451 7.7417851 178.3588942 228.8900199
## 43 44 45 46 47 48
## 25.1795750 316.7738500 414.3991879 1412.5245302 31.0933184 1219.9387043
## 49
## 1972.8451146
prepare_data
We’ll already learned that prepare_data
can join counts
and covariates into a single data.frame. It can also compute offset
through compute_offset
and does so by default with
offset = "TSS"
, hence the Offset
column in
trichoptera2
. You can change the offset method and provide
additional arguments that will passed on to
compute_offset
.
## 'data.frame': 49 obs. of 9 variables:
## $ Abundance : num [1:49, 1:17] 0 0 0 0 0 0 0 0 0 0 ...
## ..- attr(*, "dimnames")=List of 2
## .. ..$ : chr [1:49] "1" "2" "3" "4" ...
## .. ..$ : chr [1:17] "Che" "Hyc" "Hym" "Hys" ...
## $ Temperature : num 18.7 19.8 22 23 22.5 23.9 15 17.2 15.4 14.1 ...
## $ Wind : num -2.3 -2.7 -0.7 2.3 2.3 -2 -4.7 -1 -2.7 -3.7 ...
## $ Pressure : num 998 1000 997 991 990 ...
## $ Humidity : num 60 63 73 71 62 64 93 84 88 75 ...
## $ Cloudiness : num 19 0 6 81 50 50 100 19 69 6 ...
## $ Precipitation: num 0 0 0 0 0 0 1.6 0 1.6 0 ...
## $ Group : Factor w/ 12 levels "1","2","3","4",..: 1 1 1 1 1 1 1 1 1 1 ...
## $ Offset : num 0.919 0.835 0.857 0.919 0.919 ...
Different communities use different standard for the count data where
samples are either or columns of the counts matrix.
prepare_data
uses heuristics to guess the direction of the
counts matrix (or fail informatively doing so) and automatically
transpose it if needed.
Finally, prepare_data
enforces sample-consistency
between the counts and the covariates and automatically trims away: -
samples for which only covariates or only counts are available; -
samples with no positive counts
For example, if we remove the first sample from the counts and the last one from the covariates, we end up with 49 - 2 = 47 samples left, as expected.
nrow(prepare_data(trichoptera$Abundance[-1, ], ## remove first sample
trichoptera$Covariate[-49,] ## remove last sample
))
## [1] 47
prepare_data_from_[phyloseq|biom]
Community composition data are quite popular in microbial ecology and usually stored in flat files using the biom format and/or imported in R as phyloseq-class objects (McMurdie 2013) using the Bioconductor phyloseq package.
We show here how to import data from a biom file (or biom-class object) and form a phyloseq-class object.
Reading from a biom file requires the bioconductor package biomformat. This package is not a standard dependency of PLNmodels and needs to be installed separately.
You can easily prepare your data from a biom file using the following steps:
biomformat::read_biom()
biomformat::biom_data()
biomformat::sample_metadata()
(or build your own)prepare_data
as illustrated below:
## If biomformat is not installed, uncomment the following lines
# if (!requireNamespace("BiocManager", quietly = TRUE)) {
# install.packages("BiocManager")
# }
# BiocManager::install("biomformat")
library(biomformat)
biomfile <- system.file("extdata", "rich_dense_otu_table.biom", package = "biomformat")
biom <- biomformat::read_biom(biomfile)
## extract counts
counts <- as(biomformat::biom_data(biom), "matrix")
## extract covariates (or prepare your own)
covariates <- biomformat::sample_metadata(biom)
## prepare data
my_data <- prepare_data(counts = counts, covariates = covariates)
str(my_data)
Likewise, preparing data from a phyloseq-class object requires the bioconductor package phyloseq. This package is not a standard dependency of PLNmodels and needs to be installed separately.
You can easily prepare your data from a phyloseq object using the following steps:
phyloseq::otu_table()
phyloseq::sample_data()
(or
build your own)prepare_data
as illustrated below:
## If biomformat is not installed, uncomment the following lines
# if (!requireNamespace("BiocManager", quietly = TRUE)) {
# install.packages("BiocManager")
# }
# BiocManager::install("phyloseq")
library(phyloseq)
data("enterotype")
## extract counts
counts <- as(phyloseq::otu_table(enterotype), "matrix")
## extract covariates (or prepare your own)
covariates <- phyloseq::sample_data(enterotype)
## prepare data
my_data <- prepare_data(counts = counts, covariates = covariates)
str(my_data)
We detail here the mathematical background behind the various offsets and the way they are computed. Note Y = (Yij) the counts matrix where Yij is the count of species j in sample i. Assume that there are p species and n samples in total. The offset of sample i is noted Oi and computed in the following way.
Offsets are simply the total counts of a sample (frequently called depths in the metabarcoding literature): $$ O_i = \sum_{j=1}^p Y_{ij} $$
Positive counts are used to compute sample-specific quantiles qil
and cumulative sums sil
defined as qil = min {q
such that
∑j1Yij ≤ q ≥ l∑j1Yij > 0} sil = ∑j : Yij ≤ qilYij
The sample-specific quantiles are then used to compute reference
quantiles defined as ql = median{qli}
and median average deviation around the quantile ql as dl = median|qil − ql|.
The method then searches for the smallest quantile l for which it detects instability,
defined as large relative increase in the dl. Formally,
l̂ is the smallest l satisfying $\frac{d^{l+1} - d^l}{d^l} \geq 0.1$. The
scaling sample-specific offset are then chosen as: Oi = sil̂/mediani{sil̂}
Dividing by the median of the sil̂
ensures that offsets are centered around 1 and compare sizes differences with respect
to the reference sample. Note also that the reference quantiles ql can be
computed using either the median (default, as in the original Paulson et al. (2013)
paper) or the mean, by specifying reference = mean
, as
implemented in metagenomeseq
.
A reference sample (qj)j
is first built by computing the geometric means of each species count:
$$
q_j = \exp \left( \frac{1}{n} \sum_{i} \log(Y_{ij})\right)
$$ Each sample is then compared to the reference sample to
compute one ratio per species and the final offset Oi is the median
of those ratios: $$
O_i = \text{median}_j \frac{Y_{ij}}{q_j}
$$ The method fails when no species is shared across all sample
(as all qj
are then 0) or when a sample shares
less than 50% of species with the reference (in which case the median of
the ratios may be null or infinite). The problem can be alleviated by
adding pseudocounts to the cij
with pseudocounts = 1
or using positive counts in the
computations (type = "poscounts"
)
This method is similar to RLE but does create a reference sample. Instead, each sample is compared to each other to compute a median ratio (similar to RLE) $$ r_{ii'} = {\text{median}}_{j: Y_{ij}.Y_{i'j} > 0} \frac{Y_{ij}}{Y_{i'j}} $$ The offset is then taken as the median of all the rii′: Oi = mediani′! = irii′ The method fails when there is only one sample in the data set or when a sample shares no species with any other.
This method is fully detailed in Kumar et al.
(2018) and we only provide a
barebone implementation corresponding to the defaults parameters of
Wrench::wrench()
. Assume that samples belong to K discrete groups and note gi the group of
sample i. Wrench is based on
the following (simplified) log-normal model for counts: Yij ∼ πijδ0 + (1 − πij)log 𝒩(μij, σj2)
where the Yij are
independent and the mean μij is
decomposed as: $$
\mu_{ij} = \underbrace{\log{p_{0j}}}_{\text{log-ref. prop.}}
+ \underbrace{\log{d_i}}_{\text{log-depth}} +
\underbrace{\log{\zeta_{0g_i}}}_{\text{log effect of group } g_i} +
\underbrace{a_{i}}_{\text{(f|m)ixed effect}} +
\underbrace{b_{ij}}_{\text{mixed effects}}
$$ where the random effects are independents centered gaussian
and the depths is the total sum of counts: $$
\begin{align*}
d_i & = \sum_{j=1}^p c_{ij} \\
b_{ij} & \sim \mathcal{N}(0, \eta^2_{g_i}) \\
\end{align*}
$$
The net log fold change θij of the proportion ratio rij = cij/dip0j of species j relative to the reference is $\log(\theta_{ij}) \overset{\Delta}{=} \mathbb{E}[\log(r_{ij}) | a_i, b_{ij}] = \log{\zeta_{0g_i}} + a_i + b_{ij}$. We can decompose it as θij = Λi−1vij where Λi−1 is the compositional correction factor and vij is the fold change of true abundances.
With the above notations, the net fold change compounds both the fold change of true abundances and the compositional correction factors. With the assumption that the bij are centered, log (Λ̂i) can be estimated through a robust average of the θ̂ij, which can themselves be computed from the log-ratio of proportions.
We detail here how the different parameters and/or effects are estimated.
Wrench::wrench()
, the log depth
log (di)
is used as predictor but I believe it makes more sense to use it an
offset.The offsets are then the product of compositional correction factors and depths: $$ O_i = \frac{\hat{\Lambda}_i}{(\prod_{i = 1}^n \hat{\Lambda}_i)^{1/n}} \times \frac{d_i}{(\prod_{i = 1}^n d_i)^{1/n}} $$
although a data.frame
is technically a
list
↩︎