Ediacaran-type non-mineralized tube-dwelling organisms persisted into the early Cambrian (Terreneuvian) in Baltica DOI
Olev Vinn, Karma Nanglu, Mark A. Wilson

et al.

Gondwana Research, Journal Year: 2024, Volume and Issue: unknown

Published: Sept. 1, 2024

Language: Английский

Priapulid neoichnology, ecosystem engineering, and the Ediacaran–Cambrian transition DOI Creative Commons
Katherine A. Turk, Achim Wehrmann, Marc Laflamme

et al.

Palaeontology, Journal Year: 2024, Volume and Issue: 67(4)

Published: July 1, 2024

Abstract The evolutionary rise of powerful new ecosystem engineering impacts is thought to have played an important role in driving waves biospheric change across the Ediacaran–Cambrian transition (ECT; c . 574–538 Ma). Among most heavily cited these bioturbation (organism‐driven sediment disturbance) as activities been shown critical downstream geobiological impacts. In this regard priapulid worms are crucial; trace fossils left by priapulan‐grade animals now recognized appearing shortly before base Cambrian and represent some earliest examples bed‐penetrative bioturbation. Understanding priapulids may thus be key reconstructing drivers ECT. However, rare modern benthic ecosystems, comparatively little known about behaviours associated with their burrowing. Here, we present early results neoichnological experiments focused on understanding worms. We observe for first time a variety burrowing (including formation linked burrow networks long in‐burrow residence times) hinting at larger group than previously thought. Finally, identify means which contribute our tracemakers ECT, they had shaping latest Ediacaran biosphere.

Language: Английский

Citations

6

Morphology shapes community dynamics in early animal ecosystems DOI Creative Commons
Nile P. Stephenson, Katie M. Delahooke,

Nicole M. Barnes

et al.

Nature Ecology & Evolution, Journal Year: 2024, Volume and Issue: 8(7), P. 1238 - 1247

Published: June 12, 2024

Abstract The driving forces behind the evolution of early metazoans are not well understood, but key insights into their ecology and can be gained through ecological analyses in situ, sessile communities Avalon assemblage Ediacaran (~565 million years ago). Community structure is thought to underpinned by epifaunal tiering succession, which we investigate this study 18 communities. Here found that form four distinctive Types irrespective succession processes, instead based on dominance morphologically distinct taxa, prevalent three these Types. Our results consistent with emergent neutrality, whereby ecologically specialized morphologies evolve as a consequence neutral (stochastic or reproductive) processes within niches, leading generalization frond-dominated Type. provide an signature first origination subsequent loss disparate morphologies, probably community restructuring response innovation. This led survival non-tiered frondose generalists over tiered specialists, even youngest assemblages. Such body plans also survive beyond Ediacaran–Cambrian transition, perhaps due greater resilience afforded them alternative strategies.

Language: Английский

Citations

5

Photosynthetic fractionation of carbon: A biological driver for the Neoproterozoic Shuram carbon isotope excursion DOI Creative Commons

Euan N. Furness,

Emily G. Mitchell

Precambrian Research, Journal Year: 2025, Volume and Issue: 419, P. 107702 - 107702

Published: Feb. 1, 2025

Language: Английский

Citations

0

First SHRIMP Zircon U-Pb Dating Constraints for the Ediacaran Wenghui Biota DOI
Mingsheng Zhao, Feng Tang, Giovanni Mussini

et al.

Journal of Earth Science, Journal Year: 2025, Volume and Issue: 36(1), P. 102 - 112

Published: Feb. 1, 2025

Language: Английский

Citations

0

The Quanjishan Charnia assemblage from the northern Qaidam Basin, Tibetan Plateau, and implications for palaeoecology and taphonomy of Ediacaran fronds DOI

Chengxi Wu,

Alexander Liu, Yarong Liu

et al.

Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2025, Volume and Issue: unknown, P. 112816 - 112816

Published: Feb. 1, 2025

Language: Английский

Citations

0

Enigmatic discoidal macrofossils with central ring from the Ediacaran Jiangchuan biota, Southwest China DOI Open Access
Mingsheng Zhao, Yupeng Zhang, Feng Tang

et al.

Papers in Palaeontology, Journal Year: 2025, Volume and Issue: 11(2)

Published: March 1, 2025

Abstract The Jiangchuan biota is a diverse macrofossil assemblage from the Jiucheng Member of Dengying Formation, in uppermost Ediacaran (Sinian) Eastern Yunnan, Southwest China. This well known for its macroalgal fossils preserved as carbonaceous compressions, but co‐occurring taxa have remained poorly documented. Here, we present new discoidal macrofossils biota, which interpret eumetazoan‐grade organisms uncertain affinities. These disc‐like are smooth, well‐defined impressions with tube‐like peripheral zone. Most thick, three‐dimensional ring centrally, possible remnant perioral musculature and innervation. morphology these problematica invites comparison other putative Neoproterozoic medusoids Nanfen Xingmincun Formations Jilin Liaoning areas, Northeast China, enigmatic spiral‐like fossil Eoandromeda octobrachiata Doushantuoian Wenghui Guizhou. Based on shared presence central, dorsally oriented ring‐like structures fossils, speculate that annular nervous system may been widespread among organisms, it might represent plesiomorphic feature Eumetazoa.

Language: Английский

Citations

0

Two ribbon-like macrofossils in contrasting preservational styles from the Ediacaran–Cambrian interval DOI Creative Commons
Yulan Li, Giovanni Mussini, Li‐Jun Zhang

et al.

Journal of Palaeogeography, Journal Year: 2025, Volume and Issue: unknown

Published: March 1, 2025

Language: Английский

Citations

0

Ediacaran marine animal forests and the ventilation of the oceans DOI Creative Commons
Susana Gutarra,

Emily G. Mitchell,

Frances S. Dunn

et al.

Current Biology, Journal Year: 2024, Volume and Issue: 34(11), P. 2528 - 2534.e3

Published: May 17, 2024

The rise of animals across the Ediacaran-Cambrian transition marked a step-change in history life, from microbially dominated world to complex macroscopic biosphere we see today.

Language: Английский

Citations

3

Himatiichnus mangano igen. et isp. nov., a scalidophoran trace fossil from the late Ediacaran of Namibia DOI Creative Commons
Katherine A. Turk, Mikaela A. Pulsipher, Helke Mocke

et al.

Royal Society Open Science, Journal Year: 2024, Volume and Issue: 11(10)

Published: Oct. 1, 2024

Himatiichnus mangano igen. et isp. nov., a new trace fossil from the late Ediacaran Huns Member of Urusis Formation, southern Namibia, comprises intertwining tubes exhibiting dual lineation patterns and reminiscent both modern early Cambrian examples priapulid worm burrows. These similarities support interpretation total-group scalidophoran tracemaker for H. , thus providing direct evidence first appearance date Scalidophora in ca 539 Ma. This material is indicative presence scalidophorans below boundary supports inference lengthy Precambrian fuse explosion.

Language: Английский

Citations

3

A putative triradial macrofossil from the Ediacaran Jiangchuan Biota DOI Creative Commons
Mingsheng Zhao, Giovanni Mussini, Yulan Li

et al.

iScience, Journal Year: 2024, Volume and Issue: 27(2), P. 108823 - 108823

Published: Jan. 9, 2024

The late Ediacaran Jiangchuan biota, from the Dengying Formation in eastern Yunnan, is well-known for its diverse macroalgal fossils, opening a window onto eukaryotic-dominated ecosystems Neoproterozoic of South China. Although multiple lines evidence suggest that metazoans had already evolved by Ediacaran, animal fossils have not yet been formally described this locality. Here, we report putative disc-shaped macrofossil

Language: Английский

Citations

2