To evaluate the stability and resilience of coastal ecosystem communities to perturbations that occurred during the Anthropocene, pre-industrial biodiversity baselines inferred from paleoarchives are needed. The study of ancient DNA (aDNA) from sediments (sedaDNA) has provided valuable information about past dynamics of microbial species and communities in relation to ecosystem variations. Shifts in planktonic protist communities might significantly affect marine ecosystems through cascading effects, and therefore the analysis of this compartment is essential for the assessment of ecosystem variations.
View Article and Find Full Text PDFThe Holocene period (last 11,700 years BP) has been marked by significant climate variability over decadal to millennial timescales. The underlying mechanisms are still being debated, despite ocean-atmosphere-land connections put forward in many paleo-studies. Among the main drivers, involving a cluster of spectral signatures and shaping the climate of north-western Europe, are solar activity, the North Atlantic Oscillation (NAO) varying atmospheric regimes and North Atlantic oceanic gyre dynamics.
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