Abstract:The Arctic marine biome, shrinking with increasing temperature and receding sea-ice cover, is tightly connected to lower latitudes through the North Atlantic. By flowing northward through the European Arctic Corridor (the main Arctic gateway where 80% of in-and outflow takes place), the North Atlantic Waters transport most of the ocean heat, but also nutrients and planktonic organisms toward the Arctic Ocean. Using satellite-derived altimetry observations, we reveal an increase, up to two-fold, in North Atlant… Show more
“…floridanus and Sphenolithus (with high thermal optima) and demonstrating the high adaptability of the Reticulofenestra lineage to the new "baseline" conditions of the middle Miocene "icehouse world." We speculate that a regression to a warmer state of the oceans may not negatively impact highly adaptable coccolithophore taxa, such as E. huxleyi, whose poleward expansion is already evident (Oziel et al, 2020;Rivero-Calle et al, 2015;Winter et al, 2014).…”
The abundance and composition of modern phytoplankton are primarily related to equator‐to‐pole temperature gradients and global ocean circulation, which in turn determine the availability of nutrients in the photic zone. The nutricline is found at greater depths in warm, tropical waters, whereas more vigorous surface mixing in higher latitudes (seasonally) enhances nutrient availability and primary productivity. Ocean temperatures were ~7°C higher during the middle Miocene Climatic Optimum (MCO; ~16.9–14.7 million years ago, Ma), which was followed by Antarctic glaciation and global cooling during the middle Miocene Climate transition (MMCT; 14.7–13.8 Ma). Four decades ago, Haq (1980, https://doi.org.10.2307/1485353) already related migration patterns of low‐latitude versus high‐latitude calcareous nannoplankton in the Atlantic Ocean to major climatic fluctuations during the Miocene. Here, we detail and discuss the macroevolutionary patterns and processes across the middle Miocene (~16.5–11 Ma) at five deep sea sites on a north‐south transect in the Atlantic Ocean (57°N to 28°S). We show that the major cooling step toward the modern “icehouse” world impacted coccolithophore communities at all latitudes. Contrary to previous observations suggesting that tropical sites showed little change and that midlatitudes were the most sensitive recorders of climate change across the MMCT, we show that all sites recorded a marked diversification and increase in abundance of reticulofenestrids. Global cooling and related increased meridional overturning circulation are implicated as likely forcings for this macroevolutionary step toward establishing modern coccolithophore communities that are dominated by eurythermal and eurytrophic species such as Emiliania huxleyi.
“…floridanus and Sphenolithus (with high thermal optima) and demonstrating the high adaptability of the Reticulofenestra lineage to the new "baseline" conditions of the middle Miocene "icehouse world." We speculate that a regression to a warmer state of the oceans may not negatively impact highly adaptable coccolithophore taxa, such as E. huxleyi, whose poleward expansion is already evident (Oziel et al, 2020;Rivero-Calle et al, 2015;Winter et al, 2014).…”
The abundance and composition of modern phytoplankton are primarily related to equator‐to‐pole temperature gradients and global ocean circulation, which in turn determine the availability of nutrients in the photic zone. The nutricline is found at greater depths in warm, tropical waters, whereas more vigorous surface mixing in higher latitudes (seasonally) enhances nutrient availability and primary productivity. Ocean temperatures were ~7°C higher during the middle Miocene Climatic Optimum (MCO; ~16.9–14.7 million years ago, Ma), which was followed by Antarctic glaciation and global cooling during the middle Miocene Climate transition (MMCT; 14.7–13.8 Ma). Four decades ago, Haq (1980, https://doi.org.10.2307/1485353) already related migration patterns of low‐latitude versus high‐latitude calcareous nannoplankton in the Atlantic Ocean to major climatic fluctuations during the Miocene. Here, we detail and discuss the macroevolutionary patterns and processes across the middle Miocene (~16.5–11 Ma) at five deep sea sites on a north‐south transect in the Atlantic Ocean (57°N to 28°S). We show that the major cooling step toward the modern “icehouse” world impacted coccolithophore communities at all latitudes. Contrary to previous observations suggesting that tropical sites showed little change and that midlatitudes were the most sensitive recorders of climate change across the MMCT, we show that all sites recorded a marked diversification and increase in abundance of reticulofenestrids. Global cooling and related increased meridional overturning circulation are implicated as likely forcings for this macroevolutionary step toward establishing modern coccolithophore communities that are dominated by eurythermal and eurytrophic species such as Emiliania huxleyi.
“…living conditions in warming waters. Blooms of the North Atlantic calcifying algae Emiliania huxleyi have been observed to follow the ever-encroaching polar front (Neukermans et al, 2018) possibly advected there due to increased current velocities (Oziel et al, 2020).…”
Section: Changing Upper Ocean Physics Influences Geochemistry and Biomentioning
“…Under this scenario, the distribution of large long-lived generalist predators such as Copepods (Arthropoda) is expected to be stretched to the scale of currents systems through large-scale transport and mixing by main currents (Hellweger, van Sebille, & Fredrick, 2014; Lévy, Jahn, Dutkiewicz, & Follows, 2014; Madoui et al, 2017; Richter et al, 2019), and to be patchy as a result of small-scale turbulent stirring (Abraham, 1998). These contrasted views illustrate that little is known on how the interplay between body size, ecology, currents and the local environment shapes biogeography (Oziel et al, 2020).…”
Short abstractEukaryotic plankton are a core component of marine ecosystems with exceptional taxonomic and ecological diversity. Yet how their ecology interacts with the environment to drive global distribution patterns is poorly understood. Here, we use Tara Oceans metabarcoding data covering all the major ocean basins combined with a probabilistic model of taxon co-occurrence to compare the biogeography of 70 major groups of eukaryotic plankton. We uncover two main axes of biogeographic variation. First, more diverse groups display stronger biogeographic structure. Second, large-bodied consumers are structured by oceanic basins, mostly via the main currents, while small-bodied phototrophs are structured by latitude, with a comparatively stronger influence of biotic conditions. Our study highlights striking differences in biogeographies across plankton groups and disentangles their determinants at the global scale.One-sentence summaryEukaryotic plankton biogeography and its determinants at global scale reflect differences in ecology and body size.
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