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. 2023 Jun 19;9(7):1034–1043. doi: 10.1038/s41477-023-01445-6

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© The Author(s) 2023

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Extended Data Fig. 6 — Estimates of phylogenetic beta diversity are based on the species distribution models of seagrasses (n = 66 species) fitted using maximum entropy and aggregated as the variation in phylogenetic composition between sites that is, between 100 km × 100 km grid cells. Indicated are the differences in phylogenetic beta diversity across 11 marine ecoregions for four different representative concentration pathways (RCP2.6, 4.5, 6.0, and 8.5) and for two time periods T1: 2040–2050 and T2: 2090–2100. Negative values indicate reductions in phylogenetic beta diversity (that is, phylogenetic composition will become more identical) and positive values correspond to increases in beta diversity (species composition will become more dissimilar) in the future.