Taphonomy cards

Introduction to Dinosaur Fossilization

  • Dinosaurs' Transition to Fossils

    • The process from living dinosaurs to fossilized skeletons involves multiple stages.

    • Factors affecting fossilization include death, burial, and excavation.

  • Efforts in Excavation and Preparation

    • Significant effort is required to find, excavate, and prepare dinosaur bones for display.

Taphonomy

  • Definition and Importance

    • Taphonomy: The study of what happens to organisms from the time of death to when they are buried and eventually discovered.

    • Helps understand dinosaur environments, causes of death, and behaviors leading up to death.

  • Fossils Tell a Story

    • Each fossil can reveal information about the historical context in which dinosaurs lived.

Dinosaur Provincial Park

  • Location and Historical Context

    • Located in Southern Alberta, contains millions of dinosaur remnants dating back approximately 75 million years.

    • Bones found are often associated with sediments that provide context for their position and condition.

  • Correct Factors for Fossil Discoveries

    • Essential elements for fossil discoveries include:

      • Exposed Rocks: Necessary to find dinosaur bones; covered rocks limit discovery potential.

      • Age of Rocks: Rocks must be from the correct geological period (Cretaceous Period, when dinosaurs dominated).

      • Right Environment: Terrestrial sediments are preferable for dinosaur fossils since they lived on land.

      • Historical Discoveries: Previous discoveries increase the likelihood of finding additional fossils in the same area.

Glacial Influence and Erosion

  • Effect of Glaciation

    • Approximately 13,000 years ago, glaciers sculpted the landscape by scraping away younger sediments, exposing older dinosaur-bearing layers.

    • Melting glaciers created conditions for further erosion, exposing Cretaceous rocks and fossils.

  • Continued Erosion

    • Ongoing wind and rain erosion contributes to the discovery of new fossils year after year.

    • Sparse vegetation in the Badlands aids erosion, revealing more bones.

Modern Environment vs. Historical Context

  • Current Conditions

    • Dinosaur Provincial Park is too dry for new fossils to easily form.

    • Modern carcasses in the Badlands disintegrate without proper burial, preventing fossilization.

  • Past Conditions

    • The area was much wetter and more humid during the time of the dinosaurs, with rivers and wetlands providing ideal conditions for burial and fossilization.

Types of Rocks and Fossilization

  • Sedimentary Rocks

    • Composed of materials eroded from other rocks, making them ideal for fossil preservation.

    • Types include sandstones, mudstones, shales, etc., these contain sediments that can bury and preserve remains.

  • Non-Ideal Rock Types

    • Igneous Rocks: Formed from molten magma, not conducive to fossil preservation.

    • Metamorphic Rocks: Altered rocks that also do not typically contain fossils under normal circumstances.

Role of Sedimentary Geologists

  • Collaboration for Discoveries

    • Sedimentary geologists examine rock layers to identify past environments, enhancing fossil discovery strategies.

    • Preference for looking in specific sediment types (like sandstones) during searches for dinosaur fossils.