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8 results for "sulfide"

M_5_30 — Cinnabar: Mercury Sulfide in Ancient Ritual, Medicine, and Technology

Cinnabar (mercury sulfide, HgS) is a bright red mineral that served as one of the most important substances in the ancient world — prized simultaneously as a pigment, a ritual material, a medicinal ingredient, and an alc

cinnabar mercury sulfide HgS vermillion mercury alchemy

ZF_2_20 Verified Oceanography

ZF_2_20 — Submarine Volcanic Ecosystems

Submarine volcanic ecosystems — biological communities thriving at hydrothermal vents, volcanic seamounts, and submarine caldera environments — represent one of the most profound biological discoveries of the 20th centur

hydrothermal vent submarine volcano chemosynthesis extremophile black smoker deep-sea

ZF_2_17 Verified Oceanography

ZF_2_17 — Chemosynthetic Ecosystem Evolution: Life Without Sunlight

Chemosynthetic ecosystems — communities of organisms that derive energy from chemical reactions (primarily the oxidation of hydrogen sulfide, methane, or hydrogen) rather than photosynthesis — represent one of the most t

chemosynthesis hydrothermal vents cold seeps tubeworms black smokers extremophiles

ZF_2_21 Verified Oceanography

ZF_2_21 — Sargassum Bloom Crisis

The Great Atlantic Sargassum Belt (GASB) — an unprecedented, continent-spanning mass of floating Sargassum macroalgae stretching from West Africa to the Gulf of Mexico — has emerged since 2011 as one of the most dramatic

Sargassum great Atlantic Sargassum belt macroalgae bloom Caribbean nutrient loading

ZF_5_09 Verified Oceanography

ZF_5_09 — Whale Falls: Deep-Sea Decomposition and Chemosynthetic Ecosystems

Whale falls — the carcasses of large cetaceans that sink to the deep ocean floor — are among the most remarkable ecosystems in the sea, transforming the nutrient-poor desert of the abyssal plains into oases of biological

whale fall deep sea decomposition chemosynthesis sulfide bone-eating worm

ZF_4_07 Verified Oceanography

ZF_4_07 — Deep Ocean Mining and Mineral Resources

Deep-sea mining — the extraction of mineral resources from the ocean floor at depths of 200–6,000 m — is one of the most consequential and contested environmental issues in contemporary oceanography. Three primary resour

deep-sea mining polymetallic nodules manganese nodules seafloor massive sulfides cobalt-rich crusts ISA

O_3_13 Verified Earth Anomalies

O_3_13 — Hydrothermal Vents: Black Smokers and Chemosynthetic Ecosystems

Hydrothermal vents are fissures on the ocean floor — overwhelmingly concentrated along mid-ocean ridges, back-arc basins, and submarine volcanic arcs — where geothermally heated water (up to ~400°C) erupts into the frigi

hydrothermal vent black smoker white smoker chemosynthesis mid-ocean ridge deep sea

O_5_07 Verified Earth Anomalies

O_5_07 — Anoxic Events and Ocean Dead Zones: Deoxygenation Through Time

Oceanic Anoxic Events (OAEs) were episodes in Earth's history when large portions of the world's oceans became severely depleted of dissolved oxygen (anoxic) or enriched in toxic hydrogen sulfide (euxinic), causing wides

oceanic anoxic event OAE dead zone hypoxia anoxia deoxygenation

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