4.7 Review

Remarkable insights into the paleoecology of the Avalonian Ediacaran macrobiota

期刊

GONDWANA RESEARCH
卷 27, 期 4, 页码 1355-1380

出版社

ELSEVIER
DOI: 10.1016/j.gr.2014.11.002

关键词

Ediacaran; Newfoundland; Avalonia; Paleoecology; Paleontology

资金

  1. Portugal Cove South Visitor Center
  2. Natural Environment Research Council [NE/I005927/1, NE/G523539/1]
  3. Cambridge Philosophical Society
  4. National Geographic Global Exploration Fund [GEFNE 22-11]
  5. Natural Environment Research Council [1097476, NE/I005951/1, NE/I005927/1, NE/L011409/1] Funding Source: researchfish
  6. NERC [NE/L011409/1, NE/I005927/1, NE/I005951/1] Funding Source: UKRI

向作者/读者索取更多资源

Ediacaran macrofossils from the Avalon Terrane (primarily eastern Newfoundland and the central UK) record some of the earliest large and complex multicellular organisms on Earth. Perhaps the greatest unknown regarding these fossils is their relevance to the early evolutionary history of the Kingdom Animalia. In recent years, new data and discoveries have revealed insights into Ediacaran paleobiology, taxonomic relationships, paleoecology and taphonomy, significantly refining our understanding of Avalonian ecosystems. Here, we summarise recent observational and quantitative studies, and their bearing on the current understanding of Avalonian benthic marine ecosystems. A review of existing knowledge of the biological composition of Avalonian marine assemblages demonstrates that they record densely-populated ecosystems inhabited by a diverse range of organisms, likely representing multiple biological Kingdoms. Appreciation of this diversity, and of the complexities it introduces to paleoecological studies, is vital when considering the relationship between macroevolution and contemporaneous climatic tectonic and geochemical events. We then summarise current understanding of Avalonian paleoecology. Studies into locomotion, reproduction, feeding strategies, and community structure and succession reveal that these ecosystems were considerably different to Phanerozoic settings. Furthermore, we suggest that Avalonian ecosystems witnessed the appearance of novel nutrient sources, offering new opportunities and niches for benthic organisms. The suggestion that the numerically dominant rangeomorphs were osmotrophic is reviewed and appraised in light of geochemical, morphological, and biological information. Finally, the use of modem ecological metrics in the study of Ediacaran fossil assemblages is assessed. Concerns regarding the interpretation of paleoecological data are outlined in light of current taphonomic and sedimentological understanding, and these cast doubt on previous suggestions that the Avalonian assemblages were largely composed of metazoans. Nevertheless, we emphasise that if treated with necessary caution, paleoecological data can play a significant role in assisting efforts to determine the biological affinities of late Ediacaran macroscopic organisms. (C) 2014 The Authors. Published by Elsevier B.V. on behalf of International Association for Gondwana Research. This is an open access article under the CC BY license.

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