Palaeolimnological records provide valuable information about how
phytoplankton respond to long-term drivers of environmental change.
Traditional palaeolimnological tools such as microfossils and pigments
are restricted to taxa that leave sub-fossil remains, and a method that
can be applied to the wider community is required. Sedimentary DNA
(sedDNA), extracted from lake sediment cores, shows promise in
palaeolimnology, but validation against data from long-term monitoring
of lake water is necessary to enable its development as a reliable
record of past phytoplankton communities. To address this need, 18S rRNA
gene amplicon sequencing was carried out on lake sediments from a core
collected from Esthwaite Water (English Lake District) spanning
~105 years. This sedDNA record was compared with
concurrent long-term microscopy-based monitoring of phytoplankton in the
surface water. Broadly comparable trends were observed between the
datasets, with respect to the diversity and relative abundance and
occurrence of chlorophytes, dinoflagellates, ochrophytes and
bacillariophytes. Up to 20% of genera identified in the microscopy
record were also detected using sedDNA, and sedDNA revealed a previously
undetected community of phytoplankton. However, a substantial proportion
of genera identified by microscopy were not detected using sedDNA,
highlighting the current limitations of the technique that require
further development such as reference database coverage. These results
suggest that sedDNA can be used as an effective record of past
phytoplankton communities, at least over timescales of less than 100
years, but the taphonomic processes which may affect its reliability,
such as the extent and rate of deposition and DNA degradation, require
further research.