| Summary: | Harmonized data and R code for " Coherent response of zoo- and phytoplankton assemblages to global warming since the Last Glacial Maximum " by Tonke Strack, Lukas Jonkers, Marina C. Rillo, Karl-Heinz Baumann, Helmut Hillebrand and Michal Kucera (submitted to Global Ecology and Biogeography , 2024). STRUCTURED ABSTRACT Aim : We use the fossil record of different marine plankton groups to determine how their biodiversity changed during past climate warming comparable to projected future warming. Location : North Atlantic Ocean and adjacent seas. Time series cover a latitudinal range of 75°N to 6°S. Time period: Past 24,000 years, i.e., from the Last Glacial Maximum (LGM) to the current warm period covering the last deglaciation. Major taxa studied : Planktonic foraminifera, dinoflagellates and coccolithophores. Methods : We analyse time series of fossil plankton communities using principal component analysis and generalised additive models to estimate the overall trend of temporal compositional change in each plankton group and identify periods of significant change. We further analyse local biodiversity change by analysing species richness, species gains and losses, and the effective number of species in each sample and compare alpha diversity to the LGM mean. Results : All plankton groups show remarkably similar trends in the rates and spatio-temporal dynamics of local biodiversity change and a pronounced non-linearity with climate change in the current warm period. Assemblages of planktonic foraminifera and dinoflagellates started to significantly change with the onset of global warming around 15,500 to 17,000 years ago and continued to change at the same pace during the current warm period until at least 5,000 years ago, while coccolithophores assemblages changed at a constant rate throughout the past 24,000 years seemingly irrespective of the prevailing temperature change. Main conclusions : The climate change during the transition from the LGM to the current warm period led to a long-lasting reshuffling of ...
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