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Ancient Seas' Jewels

An in-depth exploration of Millericrinida, an extinct order of articulate crinoids, detailing their classification, temporal range, and evolutionary significance.

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What are Millericrinida?

Extinct Marine Echinoderms

Millericrinida represents an extinct order within the articulate crinoids, a group of marine animals belonging to the phylum Echinodermata. These fascinating creatures inhabited the Earth's oceans during specific geological epochs, leaving behind fossilized remains that offer insights into ancient marine ecosystems.

Origin and Flourishing

This order first appeared during the Anisian stage of the Middle Triassic period. Their existence spanned through the Mesozoic Era, with their lineage persisting until the Late Cretaceous period. The fossil record indicates their presence across various marine environments during this extensive timeframe.

Representative Fossil

A notable example from this order is Liliocrinus polydactylus. While visual representation is not possible here, such fossils provide critical data points for understanding the morphology and diversity of Millericrinida. These specimens are invaluable for paleontological research, helping to reconstruct the evolutionary history of crinoids.

Taxonomic Classification

Hierarchical Structure

Understanding the classification of Millericrinida places them within the broader context of the animal kingdom. Their taxonomic hierarchy is as follows:

  • Kingdom: Animalia (Multicellular, eukaryotic organisms)
  • Phylum: Echinodermata (Marine animals with radial symmetry, e.g., starfish, sea urchins)
  • Class: Crinoidea (Sea lilies and feather stars)
  • Subclass: Articulata (Crinoids with articulated skeletons)
  • Order: Millericrinida (The specific group under study)

This classification highlights their evolutionary relationships and shared characteristics with other echinoderms and crinoids.

Key Distinctions

As members of the Subclass Articulata, Millericrinida possess a skeleton composed of articulated ossicles, distinguishing them from the Inarticulata, whose skeletons are fused or unarticulated. This feature is crucial for understanding their biomechanics and fossilization potential.

Temporal Range

Mesozoic Presence

The Millericrinida order emerged during the Anisian stage of the Middle Triassic period, approximately 247 to 242 million years ago. They persisted through the Jurassic and Cretaceous periods, ultimately becoming extinct by the end of the Cretaceous, around 66 million years ago.

To contextualize their existence:

  • Middle Triassic (Anisian): This period followed the devastating Permian-Triassic extinction event. The recovery of marine ecosystems, including echinoderms, was a significant evolutionary development.
  • Late Cretaceous: This era marked the end of the Mesozoic "Age of Reptiles" and saw the K-Pg extinction event, which led to the demise of many marine groups, including the Millericrinida.

Paleoenvironmental Significance

Their presence throughout the Mesozoic indicates adaptation to diverse marine environments during a time of significant geological and biological change. Studying their fossil distribution helps paleontologists reconstruct ancient seafloor conditions and understand patterns of marine biodiversity.

Evolutionary Context

Post-Extinction Recovery

The emergence of Millericrinida in the Anisian (Middle Triassic) is particularly significant. This period witnessed a crucial recovery phase for marine fauna following the mass extinction event at the end of the Permian period. The diversification of echinoderms, including the rise of new crinoid lineages like Millericrinida, reflects the gradual rebuilding of marine biodiversity.

Research highlights the Triassic as a pivotal time for crinoid evolution. The diversification observed during this era, exemplified by groups like Millericrinida, demonstrates adaptive radiation in response to newly available ecological niches. This period was critical for establishing the patterns of marine life that would characterize subsequent geological periods.

Extinction Patterns

The extinction of Millericrinida by the end of the Cretaceous period aligns with the broader pattern of extinctions observed during the Cretaceousโ€“Paleogene (K-Pg) event. This major extinction reshaped marine ecosystems, leading to the decline of many established groups and paving the way for the rise of new forms in the Cenozoic Era.

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References

References

A full list of references for this article are available at the Millericrinida Wikipedia page

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Important Notice

This page was generated by an Artificial Intelligence and is intended for informational and educational purposes only. The content is based on a snapshot of publicly available data from Wikipedia and may not be entirely accurate, complete, or up-to-date.

This is not professional paleontological or biological advice. The information provided on this website is not a substitute for professional consultation, diagnosis, or treatment from qualified experts in paleontology, geology, or marine biology. Always seek the advice of a qualified professional with any questions you may have regarding specific scientific inquiries or research.

The creators of this page are not responsible for any errors or omissions, or for any actions taken based on the information provided herein.