By M. Gabriela Mángano, Luis A. Buatois

ISBN-10: 9401795991

ISBN-13: 9789401795999

ISBN-10: 9401796009

ISBN-13: 9789401796002

This quantity addresses significant evolutionary alterations that came about throughout the Ediacaran and the Paleozoic. those comprise discussions at the nature of Ediacaran ecosystems, in addition to the ichnologic signature of evolutionary radiations, equivalent to the Cambrian explosion and the nice Ordovician biodiversification occasion, the invasion of the land, and the end-Permian mass extinction.

This quantity set presents cutting edge stories of the main evolutionary occasions within the historical past of lifestyles from an ichnologic viewpoint. as the lengthy temporal variety of hint fossils has been regularly emphasised, biogenic buildings were often ignored in macroevolution. besides the fact that, comparisons of ichnofaunas via geologic time do demonstrate the altering ecology of organism-substrate interactions. using hint fossils in evolutionary paleoecology represents a brand new pattern that's starting a window for our knowing of significant evolutionary radiations and mass extinctions. hint fossils offer an important proof for the popularity of spatial and temporal styles and methods linked to paleoecologic breakthroughs.

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Extra resources for The Trace-Fossil Record of Major Evolutionary Events: Volume 1: Precambrian and Paleozoic

Sample text

These authors documented horizontal grooves preserved on top of beds, some of them showing transverse segments and very rarely self-overcrossing. The Fermeuse structures deserve further exploration and detailed analysis. However, the close association and apparent intergradations with the body fossil Palaeopascichnus preserved on the same bedding planes provide a cautionary note (Fig. 3a–d). The possibility that the Fermeuse structures represent a continuum of taphonomic variants of Palaeopascichnus is the most likely interpretation.

2002b), Ediacaran-like discoidal impressions and trace-like fossils were documented. The structures were subsequently reinterpreted as pseudofossils by other authors (Conway Morris 2002; Jensen 2003; Budd and Jensen 2004). However, Bengtson et al. A. G. Mángano (2007) provided a detailed description of the structures interpreted as trace fossils, which were placed in a new ichnotaxon, Myxomitodes stirlingensis. This form consists of pairs of ridges preserved in positive hyporelief and the ridges were regarded as casts of sediment-laden mucus strings.

Animals may interact with a substrate by four principal means: intrusion, compression, backfilling, and excavation (Bromley 1996; Buatois and Mángano 2011). Intrusion involves displacement of sediment as the animal moves through but the sediment closes up behind it; compression involves the movement and compaction of sediment around the animal as it passes through; backfilling involves the active backward passage of sediment either around or through the animal; and excavation comprises the active loosening and transport of sediment from one location to another (Bromley 1996; Buatois and Mángano 2011).

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The Trace-Fossil Record of Major Evolutionary Events: Volume 1: Precambrian and Paleozoic by M. Gabriela Mángano, Luis A. Buatois


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