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Marine plastic pollution is a global issue, with microplastics (1 μm–5 mm) dominating the measured plastic count1,2. Although microplastics can be found throughout the oceanic water column3,4, most studies collect microplastics from surface waters (less than about 50-cm depth) using net tows5. Consequently, our understanding of the microplastics distribution across ocean depths is more limited. Here we synthesize depth-profile data from 1,885 stations collected between 2014 and 2024 to provide insights into the distribution and potential transport mechanisms of subsurface (below about 50-cm depth, which is not usually sampled by traditional practices3,6) microplastics throughout the oceanic water column. We find that the abundances of microplastics range from 10−4 to 104 particles per cubic metre. Microplastic size affects their distribution; the abundance of small microplastics (1 μm to 100 μm) decreases gradually with depth, indicating a more even distribution and longer lifespan in the water column compared with larger microplastics (100 μm to 5,000 μm) that tend to concentrate at the stratified layers. Mid-gyre accumulation zones extend into the subsurface ocean but are concentrated in the top 100 m and predominantly consist of larger microplastics. Our analysis suggests that microplastics constitute a measurable fraction of the total particulate organic carbon, increasing from 0.1% at 30 m to 5% at 2,000 m. Although our study establishes a global benchmark, our findings underscore that the lack of standardization creates substantial uncertainties, making it challenging to advance our comprehension of the distribution of microplastics and its impact on the oceanic environment. 

Abstract Members of the order Isochrysidales are unique among haptophyte lineages in being the exclusive producers of alkenones, long‐chain ketones that are commonly used for paleotemperature reconstructions. Alkenone‐producing haptophytes are divided into three major groups based largely on molecular ecological data: Group I is found in freshwater lakes, GroupIIcommonly occurs in brackish and coastal marine environments, and GroupIIIconsists of open ocean species. Each group has distinct alkenone distributions; however, only GroupsIIandIIIIsochrysidales currently have cultured representatives. The uncultured Group I Isochrysidales are distinguished geochemically by the presence of tri‐unsaturated alkenone isomers (C_37:3bMe, C_38:3bEt, C_38:3bMe, C_39:3bEt) present in water column and sediment samples, yet their genetic diversity, morphology, and environmental controls are largely unknown. Using small‐subunit (SSU) ribosomalRNA(rRNA) marker gene amplicon high‐throughput sequencing of environmental water column and sediment samples, we show that Group I is monophyletic with high phylogenetic diversity and contains a well‐supported clade separating the previously described “EV” clade from the “Greenland” clade. We infer the first partial large‐subunit (LSU)rRNAgene Group I sequence phylogeny, which uncovered additional well‐supported clades embedded within Group I. Relative to GroupII, Group I revealed higher levels of genetic diversity despite conservation of alkenone signatures and a closer evolutionary relationship with GroupIII. In Group I, the presence of the tri‐unsaturated alkenone isomers appears to be conserved, which is not the case for GroupII. This suggests differing environmental influences on Group I andIIand perhaps uncovers evolutionary constraints on alkenone biosynthesis.