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Macroevolutionary Patterns.docx

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Biology 3466B
Yolanda Morbey

Macroevolutionary Patterns Ch. 2 & 18 pg. 689-717 / 46-48 / 61-65 How Organic Remains Fossilize Life Through Time: Fossils are traces left by organisms of the past There are Geological time scale is a hierarchy divided into eons, 4 general categories of formation: eras, periods, epochs and stages. 1. Compression: Radioisotopes and accurate dating techniques allowed Organic material buried in sediment before absolute time intervals to be assigned. decomposition leaving an impression in material below, from weight of the sediment. Phanerozoic era beings with the Cambrian Explosion and ends in the present. 2. Cast & Model: Remains decay after being buried in sediment. 3 Component Eras: Molds unfilled spaces Cast filled with new material and hardened into 1. Paleozoic (Ancient Life): rock Begins with radiation of animals, ends with mass These fossils preserve info about external and extinction at the end of the Permian. internal surfaces 2. Mesozoic (Middle Life): 3. Permineralized: Age of Reptiles beginning at the end of the Structures buried in sediment and dissolved Permian extinction and ends at the KT boundary materials precipitate into the cell. with the extinction of the dinosaurs These fossils preserve internal structure detail 3. Cenozoic (Recent Life): 4. Unaltered Remains: Age of Mammals consisting of Tertiary Period Preserved in environments that discourage loss (5 epochs) and Quaternary Period (2 epochs) from weathering. Almost all animal phyla currently recognized appeared in These fossils represent a small fraction of the fossil record, found in peat bogs, permafrost etc fossils ~40 MYA during the Cambrian Period. The fossilization process requires: 1. Durability 2. Burial Water saturated sediments 3. Lack of oxygen Strengths and Weaknesses of Fossil Record: Fossilization results in 3 types of sampling bias: 1. Geographic Propensity of fossils to come from lowland and marine habitats 2. Taxonomic Marine organisms dominate fossil record but make up 10% of extant species 3. Temporal Earths crust is being recycled, so old rocks are rarer than new. States that the ability to sample life forms should decline with time.Macroevolutionary Patterns Ch. 2 & 18 pg. 689-717 / 46-48 / 61-65 Ediacaran Fauna Phylogeny and Morphology First evidence of animals in fossils from these fauna were Lineages found at the base of the tree (Fig 18.12, 699) places around the end of the Proterozoic era (early life) predominate in the Ediacaran Fauna. Most are impression/compression fossil types without More heavily derived groups were found in the Burgess shells or hard parts Shale Fauna. Generally small in size and simple morphologically. Diploblasts / Triploblasts: Have asymmetrical or radial symmetry. Cnidaria/Ctenophora are Diploblasts, 2 embryonic tissue types. Remaining animals are Triploblasts. Fossilized embryos support hypothesis that bilaterians evolved pre-Cambrian, coming from the Doushantou Tissue types in Diploblasts: formation. 1. Ectoderm, Produce adult skin and nervous system In Doushantou rocks, phosphate minerals replaces the 2. Endoderm, Produce gut and associated organs soft tissue leaving fine anatomical details. Triploblasts have a unique Mesoderm which develop Some Ediacaran specimen qualifying as fossils are actually into gonads, heart, muscle, connective tissues and blood. Trace Fossils remnants of burrows, fecal pellets, animal tracks or other traces. The origin of diplo/triploblastsa re important because they made it possible for muscle-lined, fluid-filled cavities Burgess Shale Fauna: to evolve. Variety of large, co
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