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Vocabulary flashcards covering Earth's origin, internal structures, plate tectonics, continental drift, Cambrian paleontology, and mass extinction events based on the lecture notes.
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Earth System
An interconnected and self-regulating complex system composed of four primary components: Atmosphere (air), Hydrosphere (water), Geosphere (land), and Biosphere (life).
Gaia Theory
A hypothesis proposing that living organisms and their inorganic surroundings are closely integrated to form a self-regulating system that maintains the necessary conditions for life on the planet.
Big Bang Theory
First proposed by Georges Lemaître in the 1920s as the "hypothesis of the primeval atom," it states that the universe was once in an extremely hot, dense state that expanded rapidly.
Nebular Hypothesis
Proposed by Immanuel Kant and Pierre-Simon de Laplace in the 18th century, stating that a rotating cloud of gas and dust contracted under gravity to form the Sun and planets.
Giant Impact Hypothesis
A theory suggesting that the Moon formed from debris produced by a collision between early Earth and a Mars-sized body named Theia approximately 4.47 to 4.527 billion years ago.
Conrad Discontinuity
The seismic boundary within the continental crust that separates the upper crust (SIAL) and the lower crust (SIMA).
Mohorovičić Discontinuity
The boundary separating the Earth's crust and the upper mantle.
Repetti Discontinuity
The boundary separating the upper mantle and the lower mantle.
Gutenberg Discontinuity
The boundary separating the lower mantle and the liquid outer core.
Lehmann Discontinuity
The boundary separating the liquid outer core and the solid inner core.
Bridgmanite
The abundant mineral that predominantly composes the Earth's lower mantle.
Lithosphere
The cool, rigid, and brittle upper mechanical layer encompassing the crust and uppermost mantle.
Asthenosphere
The hot, weak, and plastic mechanical layer of the upper mantle situated directly beneath the lithosphere.
Mesosphere (Geology)
The hot but stronger layer of the lower mantle located beneath the asthenosphere, kept solid due to high pressure.
Ringwoodite
A deep-mantle mineral found as an inclusion within a 5 mm diamond, confirming the existence of vast water reservoirs trapped in Earth's deep mantle.
Continental Shelf
A shallow underwater extension of continental crust reaching depths of up to approximately 200 m.
Continental Slope
A steep transition zone leading from the continental shelf to oceanic crust, typically between 2,000 m and 3,000 m depth.
Continental Rise
A thick accumulation of sediments at the base of the continental slope leading into the abyssal plain.
Abyssal Plain
A deep, flat region of the ocean floor found at depths between 4,000 m and 6,000 m.
Pangaea
A supercontinent proposed by Alfred Wegener that existed about 200 million years ago before breaking apart into the modern continents.
Seafloor Spreading
A concept proposed by Harry Hess in 1962 stating that new oceanic seafloor is continually generated at mid-oceanic ridges as magma rises from the mantle.
Slab Pull
The primary driver of tectonic plate motion, where cold, dense ocean lithosphere sinks into a subduction zone under gravity.
Ridge Push
A force driving plate movement caused by the gravitational sliding of lithosphere away from an elevated mid-ocean ridge.
Wilson Cycle
The cyclical opening and closing of ocean basins driven by continental rifting, ocean formation, subduction initiation, terrane accretion, mountain building, and erosion.
Philippine Mobile Belt
A complex, highly active tectonic boundary zone squeezed between the Eurasian/Sundaland Plate and the Philippine Sea Plate.
Cambrian Explosion
A major evolutionary event occurring between 542 and 496 Ma, characterized by the sudden appearance and rapid diversification of most major animal phyla.
Burgess Shale
A famous Middle Cambrian fossil locality in the Canadian Rocky Mountains, discovered by Charles D. Walcott in 1909, known for its exceptional preservation of soft-bodied organisms.
Marrella
A small arthropod-like organism resembling a trilobite, recognized as one of the most common Burgess Shale fossils and likely the first soft-bodied organism noticed by Walcott.
Anomalocaris
An apex predator of the Burgess Shale reaching up to 1 m in length, featuring compound eyes with up to 16,000 lenses, 11 pairs of swimming flaps, and a mouth with 32 teeth-like plates.
Aegirocassis benmoulae
A giant filter-feeding relative of Anomalocaris featuring dorsal and ventral flaps, recognized as the largest animal of its era.
Opabinia
A bizarre Burgess Shale organism possessing five eyes and a flexible nozzle or proboscis resembling a vacuum cleaner hose.
Hallucigenia
A Burgess Shale animal with a distinct body plan featuring seven pairs of walking spines.
Wiwaxia
A slug-like Burgess Shale organism covered in overlapping armor plates and two rows of longer, upward-projecting spines.
Pikaia
One of the earliest known primitive chordates found in the Burgess Shale fossil site.
Ottoia
A carnivorous priapulid ("penis worm") that lived in burrowed sediments and represents one of the most abundant worms in the Burgess Shale.
Index Fossil
A fossil species characterized by morphological distinctiveness, wide geographic distribution, and a narrow stratigraphic range used to identify and date the rock layer in which it is found.
Permian-Triassic Extinction
The most severe mass extinction event in paleontological history, wiping out 96 to 97% of all fossil species, 70% of land organisms, and causing the final extinction of trilobites.
Saurischian
"Lizard-hipped" dinosaurs, comprising Theropods (such as Tyrannosaurus rex) and Sauropods (such as Apatosaurus).
Ornithischian
"Bird-hipped" herbivorous dinosaurs, including species such as Stegosaurus, Triceratops, and Ankylosaurus.
Archaeopteryx
A Late Jurassic transitional fossil displaying dinosaurian features (teeth, long tail) alongside avian features (feathers, wishbone), proving birds evolved from saurischian dinosaurs.
Chicxulub Crater
A massive impact crater located in Mexico's Yucatán Peninsula formed by a bolide impact approximately 65.5 million years ago, driving the K-T mass extinction.
Shocked Quartz
Quartz crystals displaying shock lamellae created by extreme pressure, serving as geological proof of a meteorite impact.
Tektites
Natural glass bodies formed from terrestrial material melted during an impact event and rapidly cooled in the atmosphere.
Overkill Hypothesis
A theory suggesting that late Pleistocene megafaunal extinctions were primarily caused by overpredation by expanding early human populations.
Plastiglomerate
A novel rock type composed of natural sedimentary debris fused together by melted plastic, symbolic of human impact in the Anthropocene epoch.