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144 results for "climate cooling" — page 7 of 8
ZF_1_00 — Physical Oceanography: Subfolder Summary
ZF_0_00 — Oceanography & Marine Science: Section Summary
E_3_15 — Sea-Level Curves: Eustatic Change from LGM to Present
Sea-level curves — graphical reconstructions of how global mean sea level has changed through time — represent one of the most important datasets in Quaternary science, recording the waxing and waning of continental ice
E_3_21 — The 5.9 Kiloyear Event: Saharan Desiccation & the Birth of River Civilizations
The 5.9 kiloyear event (c. 3900 BCE) marks the terminal phase of the African Humid Period — a 6,000-year interval during which the Sahara was a grassland savanna supporting abundant lakes, rivers, and human populations.
E_3_18 — Black Mat: Younger Dryas Boundary Layer Geochemistry
The "black mat" is a thin, dark, organic-rich sedimentary layer found at dozens of archaeological and geological sites across North America, dating to the onset of the Younger Dryas stadial (~12,800 cal BP). First system
E_2_13 — Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM) — approximately 55.8 million years ago — was the most extreme rapid warming event of the past 66 million years and is widely studied as a deep-time analog for modern anthropoge
E_4_00 — Dating Chronological Science: Subfolder Summary
E_4_23 — Magnetic Field Strength History: Dipole Decay and Implications
Earth's magnetic field — generated by convective motion of liquid iron in the outer core (the geodynamo) — is not constant in strength. Over the past ~170 years of direct measurement (since Carl Friedrich Gauss's first s
E_1_15 — Uranium-Thorium Dating: Methodology and Applications in Deep Time
Uranium-thorium (U-Th) dating, also called uranium-series disequilibrium dating, is a radiometric technique that measures the decay of ²³⁴U to ²³⁰Th (half-life: ~245,620 years) in materials such as speleothems (cave form
E_1_16 — Thera/Santorini Eruption: Detailed Analysis of the Minoan Catastrophe
The eruption of Thera (modern Santorini, Greece) was one of the largest volcanic events in the Holocene — estimated at VEI 6–7 (Volcanic Explosivity Index), ejecting approximately 30–80 km³ of magma (dense rock equivalen
E_1_09 — Solar Storms and Miyake Events
The Sun periodically releases enormous bursts of energy — coronal mass ejections (CMEs) and solar proton events (SPEs) — that interact with Earth's magnetosphere and can have devastating consequences for technology-depen
E_1_00 — Impact Space Catastrophes: Subfolder Summary
E_0_00 — Cataclysms & Chronology: Section Summary
E_5_06 — Holocene Sixth Mass Extinction: Current Biodiversity Crisis
The Holocene "Sixth Mass Extinction" hypothesis holds that current species loss rates are 100–1,000 times the normal background extinction rate, driven primarily by human activity: habitat destruction, overexploitation,
E_5_02 — The Ordovician-Silurian Mass Extinction
The Late Ordovician mass extinction (c. 445–444 million years ago, at the Ordovician-Silurian boundary) was the second-most severe extinction event in Earth's history in terms of percentage of species lost — approximatel
ZB_3_23 — Coral Reef Ecosystem Dynamics
Coral reefs are among Earth's most biodiverse and economically valuable ecosystems, occupying less than 0.1% of the ocean floor yet supporting approximately 25% of all marine species (~830,000 species). Built over millen
ZB_3_11 — Tropical Rainforest Ecology: Earth's Richest Biome
Tropical rainforests — evergreen broadleaf forests occurring in equatorial zones receiving >2,000 mm annual rainfall with no pronounced dry season and temperatures averaging 25–27°C year-round — cover approximately 6–7%
O_5_16 — Gaia Hypothesis and Earth System Self-Regulation
The Gaia hypothesis, proposed by James Lovelock (atmospheric chemist, 1919–2022) and co-developed with Lynn Margulis (microbiologist, 1938–2011), posits that Earth's biosphere, atmosphere, oceans, and geosphere interact
O_5_20 — Enceladus: Saturn's Ocean Moon and the Search for Extraterrestrial Life
Enceladus, a small icy moon of Saturn (504 km diameter, roughly the size of Arizona), has emerged since the Cassini mission's discoveries (2005–2017) as arguably the most promising location in the solar system for the de
O_5_19 — Pacific Ocean Anomalies: Ring of Fire, Deep-Sea Mysteries, and Tectonic Frontiers
The Pacific Ocean — Earth's largest and deepest body of water — concentrates a disproportionate share of geological anomalies. The Ring of Fire encircles it with 75% of the world's active volcanoes and 90% of earthquakes
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