The Rise of Animals in a Changing Environment: Global Ecological Innovation in the Late Ediacaran
Open accessAbstract
The evolutionary trajectory of early complex life on Earth is interpreted largely from the fossils of the Precambrian soft-bodied Ediacara Biota, which appeared and evolved during a time of dynamic biogeochemical and environmental fluctuation in the global ocean. The Ediacara Biota is historically divided into three successive Assemblages—the Avalon, the White Sea, and the Nama—which are marked by the appearance of novel biological traits and ecological strategies. In particular, the younger White Sea and Nama Assemblages record a “second wave” of ecological innovations, which included not only the development of uniquely Ediacaran body plans and ecologies, such as matground adaptations, but also the dual emergence of bilaterian-grade animals and Phanerozoic-style ecological innovations, including spatial heterogeneity, complex reproductive strategies, ecospace utilization, motility, and substrate competition. The late Ediacaran was an evolutionarily dynamic time characterized by strong environmental control over the distribution of taxa in time and space.
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Both the diversity and taxonomic disparity of macroscopic soft-bodied organisms increase significantly after ~560 Ma.
“but both the diversity and taxonomic disparity of macroscopic soft-bodied organisms increase significantly after ~560 Ma (3,60).”
From Integrated records of environmental change and evolution challenge the Cambrian Explosion (2019) · cites this paper as [3]
The White Sea Assemblage section reports a wide range of new taxa and pronounced increases in body-plan diversity in younger Ediacaran assemblages. The section on second-wave innovation also describes many novel morphologies relative to the older Avalon Assemblage. The paper does not establish ~560 Ma as the threshold for that increase, and it notes a subsequent reduction in diversity with the Nama Assemblage. Page numbers were not available in our copy. (LLM, conf=0.83)
Experimental — accuracy not yet measuredA literal reading of the record shows the main decrease in soft-bodied benthic biodiversity to have occurred ~5-10 Myr prior to the Ediacaran-Cambrian boundary.
“A literal reading of the record shows the main decrease in soft-bodied benthic biodiversity to have occurred ~5-10 Myr prior to the Ediacaran-Cambrian boundary (3,85).”
From Integrated records of environmental change and evolution challenge the Cambrian Explosion (2019) · cites this paper as [3]
The White Sea Assemblage section reports a notable reduction in diversity with the appearance of the Nama Assemblage, and the Discussion places the disappearance of most Ediacara taxa before the Cambrian. The copy does not establish that the main decrease occurred specifically 5–10 million years before the boundary; it also cautions that the apparent reduction may reflect preservation or environmental differences. (LLM, conf=0.83)
Experimental — accuracy not yet measuredIn the post-glacial Ediacaran (635 to 541 Ma), macroscopic body fossils at ~570 Ma were followed by a great diversity of often large, dominantly soft-bodied animals, including bilaterians, and parallel advances in ecological complexity between ~570 Ma and the Precambrian-Cambrian boundary.
“We then jump to the post-glacial Ediacaran (635 to 541 Ma), with macroscopic body fossils at ∼570 Ma (Pu et al., 2016; rangeomorphs often, though not universally, assumed to be animals) followed by a great diversity of often large, dominantly soft-bodied animals, including bilaterians, and parallel advances in ecological complexity between ∼570 Ma and the Precambrian-Cambrian boundary (reviewed in”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Droser et al., 2017
Ediacaran body fossils are limited to the interval between ~570 Ma and the base of the Cambrian roughly 30 million years later.
“Despite the extraordinary array of early animals and lifestyles on display, the Ediacaran body fossils are limited to the interval between ∼570 Ma and the base of the Cambrian roughly 30 million years later (reviewed in Xiao and Laflamme, 2009; Droser et al., 2017; Darroch et al., 2018).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Droser et al., 2017
The latter part of the Ediacaran witnessed impressive diversification among the animals and corresponding ecosystem complexity, including the emergence of bilaterians, large mostly soft body plans, the earliest infaunal activity, mobility, advances in heterotrophy, possible stem-group molluscs, and even the first skeletons.
“The latter part of the Ediacaran witnessed impressive diversification among the animals and corresponding ecosystem complexity, including the emergence of bilaterians, large mostly soft body plans, the earliest infaunal activity, mobility, advances in heterotrophy, possible stem-group molluscs, and even the first skeletons (reviewed in Droser et al., 2017).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Droser et al., 2017
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“Despite the extraordinary array of early animals and lifestyles on display, the Ediacaran body fossils are limited to the interval between *570 Ma and the base of the Cambrian roughly 30 million years later (reviewed in Xiao and Laflamme, 2009; Droser et al., 2017; Darroch et al., 2018).”
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Self-citationCauses and consequences of end-Ediacaran extinction – an update
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The trilobite upper limb branch is a well-developed gill
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Huang, W., Tarduno, J. A., Zhou, T., Ibáñez-Mejía, M., Olmo‐Barbosa, L. D., Koester, E., Blackman, E. G., Smirnov, A. V., Ahrendt, G. C., Cottrell, R. D., et al. (2024) · Communications Earth & Environment · doi:10.1038/s43247-024-01360-4 · Cited by 34 · see citing works
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Following the logic behind biological interpretations of the Ediacaran biotas
Runnegar, B. N. (2021) · Geological Magazine · doi:10.1017/s0016756821000443 · Cited by 32 · see citing works
Mussini, G., & Dunn, F. S. (2023) · Biological reviews/Biological reviews of the Cambridge Philosophical Society · doi:10.1111/brv.13014 · Cited by 31 · see citing works
Developmental capacity and the early evolution of animals
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Arrouy, M. J., Gaucher, C., Poiré, D. G., Xiao, S., Gómez-Peral, L. E., Warren, L. V., Bykova, N., & Quaglio, F. (2019) · Journal of South American Earth Sciences · doi:10.1016/j.jsames.2019.05.015 · Cited by 32 · see citing works
Palaeolatitudinal distribution of the Ediacaran macrobiota
Boddy, C. E., Mitchell, E. G., Merdith, A., & Liu, A. (2021) · Journal of the Geological Society · doi:10.1144/jgs2021-030 · Cited by 30 · see citing works
Bottom-up controls, ecological revolutions and diversification in the oceans through time
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Widespread seafloor anoxia during generation of the Ediacaran Shuram carbon isotope excursion
Ostrander, C. M., Bjerrum, C. J., Ahm, A. C., Stenger, S. R., Bergmann, K., El‐Ghali, M. A. K., Harthi, A. R., Aisri, Z., & Nielsen, S. G. (2023) · Geobiology · doi:10.1111/gbi.12557 · Cited by 29 · see citing works
Arumberia and other Ediacaran–Cambrian fossils of central Australia
Retallack, G. J., & Broz, A. (2020) · Historical Biology · doi:10.1080/08912963.2020.1755281 · Cited by 28 · see citing works
Probable benthic macroalgae from the Ediacara Member, South Australia
Xiao, S., Gehlîng, J. G., Evans, S. D., Hughes, I. V., & Droser, M. L. (2020) · Precambrian Research · doi:10.1016/j.precamres.2020.105903 · Cited by 29 · see citing works
Self-citationDroser, M. L., Tarhan, L. G., Evans, S. D., Surprenant, R., & Gehlîng, J. G. (2020) · Interface Focus · doi:10.1098/rsfs.2019.0100 · Cited by 27 · see citing works
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Life on the Edge: The Cambrian Marine Realm and Oxygenation
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Feng, X., Chen, Z., Bottjer, D. J., Wu, S., Zhao, L., Ya-ling, X., Shi, G. R., Huang, Y., Fang, Y., & Tu, C. (2018) · Earth-Science Reviews · doi:10.1016/j.earscirev.2018.07.012 · Cited by 26 · see citing works
Developmental processes in Ediacara macrofossils
Evans, S. D., Droser, M. L., & Erwin, D. H. (2021) · Proceedings of the Royal Society B Biological Sciences · doi:10.1098/rspb.2020.3055 · Cited by 25 · see citing works
Self-citationThe oldest record of Ediacaran macrofossils in Gondwana (~563 Ma, Itajaí Basin, Brazil)
Becker-Kerber, B., Paim, P. S. G., Chemale, F., Girelli, T. J., da Rosa, A. L. Z., Albani, A. E., Osés, G. L., Prado, G., Figueiredo, M. F., Simões, L. S. A., et al. (2020) · Gondwana Research · doi:10.1016/j.gr.2020.03.007 · Cited by 25 · see citing works
Wan, B., Chen, Z., Yuan, X., Pang, K., Tang, Q., Guan, C., Wang, X., Pandey, S. K., Droser, M. L., & Xiao, S. (2020) · Gondwana Research · doi:10.1016/j.gr.2020.04.003 · Cited by 26 · see citing works
Self-citationEvents in Early Nervous System Evolution
Paulin, M. G., & Cahill‐Lane, J. (2021) · Topics in Cognitive Science · doi:10.1111/tops.12461 · Cited by 35 · see citing works
Evans, S. D., Dzaugis, P. W., Droser, M. L., & Gehlîng, J. G. (2018) · Australian Journal of Earth Sciences · doi:10.1080/08120099.2018.1470110 · Cited by 24 · see citing works
Self-citationLi, D.-D., Zhang, X., Hu, D., Li, D., Zhang, G., Zhang, X., Ling, H.-F., Xu, Y., & Shen, Y.-N. (2020) · Precambrian Research · doi:10.1016/j.precamres.2019.105500 · Cited by 21 · see citing works
La transición ediacárico-cámbrica: facies sedimentarias versus extinción
Gehlîng, J. G., García‐Bellido, D. C., Droser, M. L., Tarhan, M. L., & Runnegar, B. N. (2019) · Estudios Geológicos · doi:10.3989/egeol.43601.554 · Cited by 24 · see citing works
Self-citationSurprenant, R., Gehlîng, J. G., & Droser, M. L. (2020) · Palaios · doi:10.2110/palo.2020.014 · Cited by 23 · see citing works
Self-citationMulling and nulling the coeval rise of Ediacaran oxygen and animals
Ostrander, C. M. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118187 · Cited by 24 · see citing works
Tarduno, J. A., Zhou, T., Huang, W., & Jodder, J. (2025) · National Science Review · doi:10.1093/nsr/nwaf082 · Cited by 22 · see citing works
Zhang, L., Chang, S., Chen, C., Wang, X., Feng, Q., Steiner, M., Yang, B., Mason, R., She, Z., Yan, J., et al. (2022) · Precambrian Research · doi:10.1016/j.precamres.2021.106552 · Cited by 22 · see citing works
Yi, Y., Chen, F., Algeo, T. J., & Feng, Q. (2022) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2022.110878 · Cited by 22 · see citing works
Agić, H., Högström, A. E. S., Moczydłowska, M., Jensen, S., Palacios, T., Meinhold, G., Ebbestad, J. O. R., Taylor, W. L., & Høyberget, M. (2019) · Scientific Reports · doi:10.1038/s41598-019-50650-x · Cited by 21 · see citing works
The Ediacaran frondose fossilArboreafrom the Shibantan limestone of South China
Wang, X., Pang, K., Chen, Z., Wan, B., Xiao, S., Zhou, C., & Yuan, X. (2020) · Journal of Paleontology · doi:10.1017/jpa.2020.43 · Cited by 21 · see citing works
From organisms to biodiversity: the ecology of the Ediacaran/Cambrian transition
Mitchell, E. G., & Pates, S. (2025) · Paleobiology · doi:10.1017/pab.2024.21 · Cited by 21 · see citing works
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The Ediacaran fossils of Charnwood Forest: Shining new light on a major biological revolution
Kenchington, C. G., Harris, S., Vixseboxse, P. B., Pickup, C., & Wilby, P. R. (2018) · Proceedings of the Geologists Association · doi:10.1016/j.pgeola.2018.02.006 · Cited by 19 · see citing works
The short-lived but successful tri-radial body plan: a view from the Ediacaran of Australia
Hall, C. M. S., Droser, M. L., Clites, E. C., & Gehlîng, J. G. (2018) · Australian Journal of Earth Sciences · doi:10.1080/08120099.2018.1472666 · Cited by 20 · see citing works
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Huang, K., Cheng, M., Algeo, T. J., Hu, J., Wang, H., Zhang, Z., Dodd, M. S., Wu, Y., Guo, W., & Li, C. (2022) · Precambrian Research · doi:10.1016/j.precamres.2022.106814 · Cited by 19 · see citing works
Microbially induced sedimentary structures from the Ediacaran of Anti-Atlas, Morocco
Kabouri, J. E., Errami, E., Becker-Kerber, B., Ennih, N., & Youbi, N. (2023) · Precambrian Research · doi:10.1016/j.precamres.2023.107135 · Cited by 18 · see citing works
Wu, C., Pang, K., Chen, Z., Wang, X., Zhou, C., Wan, B., Yuan, X., & Xiao, S. (2022) · Journal of Paleontology · doi:10.1017/jpa.2022.97 · Cited by 18 · see citing works
Chronology of Ediacaran sedimentary and biogeochemical shifts along eastern Gondwanan margins
Cantine, M. D., Rooney, A. D., Knoll, A. H., Gómez-Pérez, I., Baloushi, B., & Bergmann, K. (2024) · Communications Earth & Environment · doi:10.1038/s43247-024-01630-1 · Cited by 19 · see citing works
The Importance of Size and Location Within Gregarious Populations of Ernietta plateauensis
Gibson, B. M., Darroch, S. A. F., Maloney, K. M., & Laflamme, M. (2021) · Frontiers in Earth Science · doi:10.3389/feart.2021.749150 · Cited by 18 · see citing works
Tarhan, L. G., Pippenger, K. H., Cribb, A. T., Zill, M. E., Phelps, W., Droser, M. L., Bottjer, D. J., & Clapham, M. E. (2025) · Science Advances · doi:10.1126/sciadv.adu7719 · Cited by 17 · see citing works
Self-citationRevisiting the Biological Ramifications of Variations in Earth’s Magnetic Field
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Boan, P. C., Evans, S. D., Hall, C. M. S., & Droser, M. L. (2023) · Paleobiology · doi:10.1017/pab.2023.9 · Cited by 16 · see citing works
Self-citationThe Ediacara Member, South Australia: Lithofacies and palaeoenvironments of the Ediacara biota
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Ediacaran diversity and paleoecology from central Iran
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The slow rise of complex life as revealed through biomarker genetics
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Precambrian Earth: Co-evolution of life and geodynamics
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Vanadium isotope evidence for expansive ocean euxinia during the appearance of early Ediacara biota
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Boan, P. C., Evans, S. D., & Droser, M. L. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104467 · Cited by 13 · see citing works
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Kabouri, J. E., Errami, E., Bowyer, F. T., Becker-Kerber, B., & Belkacim, S. (2024) · Earth-Science Reviews · doi:10.1016/j.earscirev.2024.105010 · Cited by 11 · see citing works
Agić, H., Högström, A. E. S., Jensen, S., Ebbestad, J. O. R., Vickers-Rich, P., Hall, M., Matthews, J. J., Meinhold, G., Høyberget, M., & Taylor, W. L. (2021) · Geological Magazine · doi:10.1017/s0016756821001096 · Cited by 11 · see citing works
Tarhan, L. G., Droser, M. L., & Gehlîng, J. G. (2021) · Precambrian Research · doi:10.1016/j.precamres.2021.106539 · Cited by 11 · see citing works
Self-citationDid high temperature rather than low O2 hinder the evolution of eukaryotes in the Precambrian?
Zhang, F., Wang, H., Ye, Y., Liu, Y., Lyu, Y., Deng, Y., Lyu, D., Wang, X., Wu, H., Deng, S., et al. (2022) · Precambrian Research · doi:10.1016/j.precamres.2022.106755 · Cited by 11 · see citing works
- Authors
- Droser, M. L., Tarhan, L. G., & Gehling, J. G.
- Affiliations
- University of California, Riverside (US)
- Yale University (US)
- South Australia Museum, North Terrace, Adelaide, South Australia 5000, Australia;
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 2017-08-30
- Volume
- 45
- Issue
- 1
- Pages
- 593-617
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2592803045
- Semantic Scholar
- 2cb246bf81e209e56705c780b75394a0ae6d525d
- Cited by
- 172
- References
- 149
- Citations by year
- 2026: 17 · 2025: 18 · 2024: 19 · 2023: 16 · 2022: 17 · 2021: 22 · 2020: 23 · 2019: 16 · 2018: 19 · 2017: 5
- FWCI
- 2.13
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Annual Review of Earth and Planetary Sciences (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- Funders
- National Science Foundation
- National Aeronautics and Space Administration (NNG04GJ42G)
- National Geographic Society
- Australian Research Council (DP0453393)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Keywords
- Ediacara biota, Late Ediacaran, early animal evolution, green innovation, environmental change, spatial heterogeneity, reproductive strategies, motility, substrate competition, soft-bodied fossils
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