Early Cambrian phytoplankton diversification and appearance of trilobites in the Swedish Caledonides with implications for coupled evolutionary events between primary producers and consumers

The newly examined Lower Cambrian strata in the Laisvall‐Storuman area, central Swedish Caledonides, yield diverse and stratigraphically significant phytoplanktic organic‐walled microfossils (acritarchs) associated with the olenellid trilobites of Holmia sp. that appear to be at the lowermost horizon ever recorded in the Caledonides. The acritarchs, recovered throughout the Grammajukku Formation, are taxonomically reviewed in the context of regional and global trends of phytoplankton diversity. The assemblages are assigned to acritarch zones Skiagia ornata‐Fimbriaglomerella membranacea and Heliosphaeridium dissimilare‐Skiagia ciliosa, corresponding to the Schmidtiellus mickwitzi and Holmia kjerulfi trilobite zones. The records of acritarch radiations and appearances of trilobites and other faunas in Baltica, and on a more interregional scale, are biochronologically correlated, revealing tightly coupled evolutionary events among primary producers and consumers. The timing of early diversifications of trilobites in various faunal provinces is discussed and the relative age of the oldest known non‐mineralized arthropods from the Zawiszyn Formation in Poland is estimated.