The aforementioned illustration also includes org-I (gas) and
org-I (solid) in the marine sediment layer. It is thought that the settlement of iodine-rich organic matter derived from marine plants on the
seafloor results in the accumulation of iodine in the marine sediment. High
concentrations of iodine are accumulated, as observed during the observation of methane gas layers deep underground in the Pacific coastal area
of Chiba Prefecture. The large quantity of marine plants containing iodine that
settled long ago is thought to be a reason for this accumulation. Some of this
is thought to be organic iodine (org-I) because this iodine is present
in sediments rich with organic matter. Therefore, we showed org-I (solid)
as well, based on these assumptions.
Our laboratory has firstly measured the organic iodine gas (org-I (gas)) in the sediment (began in
2018). We have been finding a lot mysteries about org-I gas in the sediment.