bioRxiv · 10.1101/2020.04.30.068601
Short-term responses to ocean acidification: effects on relative abundance of eukaryotic plankton from the tropical Timor Sea
Abstract
Anthropogenic carbon dioxide (CO2) emissions drive climate change and pose one of the major challenges of our century. The effects of increased CO2 in the form of ocean acidification (OA) on the communities of marine planktonic eukaryotes in tropical regions such as the Timor Sea are barely understood. Here, we show the effects of high CO2 (pCO2=1823{+/-}161 atm, pHT=7.46{+/-}0.05) versus in situ CO2 (pCO2=504{+/-}42 atm, pHT=7.95{+/-}0.04) seawater on the community composition of marine planktonic eukaryotes immediately and after 48 hours of treatment exposure in a shipboard microcosm experiment. Illumina sequencing of the V9 hypervariable region of 18S rRNA (gene) was used to study the eukaryotic community composition. Down-regulation of extracellular carbonic anhydrase occurred faster in the high CO2 treatment. Increased CO2 significantly suppressed the relative abundances of different eukaryotic operational taxonomic units (OTUs), including important primary producers. These effects were consistent between abundant (DNA-based) and active (cDNA-based) taxa after 48 hours, e.g., for the diatoms Trieres chinensis and Stephanopyxis turris. Effects were also very species-specific among different diatoms. Planktonic eukaryotes showed adaptation to the CO2 treatment over time, but many OTUs were adversely affected by decreasing pH. OA effects might fundamentally impact the base of marine biodiversity, suggesting profound outcomes for food web functioning in the future ocean.
Source connections
Explore related subjects
Keep this discovery
Explore connections, maps & timelines
Rahlff, J., Khodami, S., Voskuhl, L., Humphreys, M., Stolle, C., Martinez Arbizu, P., Wurl, O., Ribas-Ribas, M.. 2020-05-02. Short-term responses to ocean acidification: effects on relative abundance of eukaryotic plankton from the tropical Timor Sea. https://doi.org/10.1101/2020.04.30.068601
Cite the original work for its findings. Save a collection to share your selection of sources.