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36 results for "domoic acid" — page 1 of 2
ZF_4_14 — Harmful Algal Blooms: Red Tides, Toxins, and Eutrophication
Harmful algal blooms (HABs) — rapid proliferations of microscopic algae (phytoplankton) or cyanobacteria that produce toxins, deplete oxygen, or otherwise damage marine ecosystems, fisheries, and human health — are incre
L_5_14 — Amino Acid Racemization Dating Method
Amino acid racemization (AAR) — a geochronological dating technique based on the chemical conversion of L-amino acids (the biologically predominant enantiomer in living organisms) to D-amino acids (the mirror-image confi
ZF_4_08 — Ocean Acidification Paleoclimate Record
Ocean acidification — the decrease in seawater pH caused by absorption of atmospheric CO₂ — is not only a modern phenomenon but has occurred repeatedly throughout Earth's history, leaving distinctive signals in the geolo
ZF_4_01 — Ocean Acidification and Marine Chemistry
The global ocean has absorbed approximately 30% of anthropogenic CO₂ emissions since the Industrial Revolution and over 90% of excess heat from the enhanced greenhouse effect, making it the planet's primary climate buffe
ZB_2_25 — Short-Chain Fatty Acids: Microbial Metabolites and Host Signaling
Short-chain fatty acids (SCFAs) — predominantly acetate (C2), propionate (C3), and butyrate (C4) — are the principal metabolites produced by anaerobic bacterial fermentation of dietary fiber in the mammalian colon, reach
R_1_15 — The Chirality Problem: Why Life Uses Left-Handed Amino Acids
One of the deepest unsolved problems in the origin of life is homochirality — the fact that all known life on Earth uses almost exclusively L-amino acids (left-handed) for proteins and D-sugars (right-handed) for nucleic
E_5_03 — The End-Triassic Mass Extinction
The End-Triassic mass extinction (c. 201.564 ± 0.015 million years ago) was one of the "Big Five" mass extinctions in Earth's history, eliminating approximately 76% of all species and ~50% of genera, clearing the ecologi
R_5_11 — Coral Biology: Symbiosis, Bleaching, and Reef Building
Coral reefs — often called the "rainforests of the sea" — are among Earth's most biodiverse and productive ecosystems, occupying less than 0.1% of the ocean floor yet supporting approximately 25% of all marine species. T
M_3_12 — Stone Softening Claims: Mythological and Chemical Analysis
Among the most intriguing and elusive claims in alternative archaeology is the idea that ancient Andean peoples possessed a botanical or chemical method of "softening" stone — reducing hard stone (particularly the andesi
M_1_12 — Ancient Electrical Phenomena: Baghdad Battery and Electroplating
The "Baghdad Battery" (also called the Parthian Battery) refers to a set of artifacts discovered in 1936 at Khujut Rabu (near Baghdad, Iraq) by German archaeologist Wilhelm König, then Director of the Baghdad Museum. The
X_5_17 — Gastroenterology and Microbiome Medicine
Gastroenterology — the study of the gastrointestinal (GI) tract and its diseases — has been revolutionized by two discoveries: the role of Helicobacter pylori in peptic ulcer disease (Barry Marshall and Robin Warren, 198
ZF_5_12 — Paleocene-Eocene Thermal Maximum: Ancient Anoxic Ocean Crisis
The Paleocene-Eocene Thermal Maximum (PETM), occurring approximately 55.8 million years ago (latest Paleocene), was one of the most dramatic and rapid climate change events in the Cenozoic, offering the closest geologica
ZF_5_16 — Ocean Observation Networks: Global Monitoring of the Marine Environment
Ocean observation networks constitute the global infrastructure for monitoring the physical, chemical, and biological state of the world's oceans in near-real-time. The centerpiece of modern ocean observation is the Argo
Z_5_11 — Microbiome-Host Coevolution: Holobiont Theory, Gut Ecology, and Metabolic Symbiosis
Microbiome-host coevolution refers to the deep, reciprocal evolutionary relationship between multicellular organisms and the complex microbial communities (bacteria, archaea, fungi, viruses) that inhabit their bodies — p
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_2_04 — Permian-Triassic Great Dying — The Biggest Mass Extinction
Approximately 252 million years ago, at the boundary between the Permian and Triassic periods, Earth experienced the worst mass extinction in its entire history — an event so devastating it has been called "The Great Dyi
Q_3_09 — Astrobiology and Origin of Life in Space
Astrobiology — the study of the origin, evolution, distribution, and future of life in the universe — sits at the intersection of biology, chemistry, planetary science, and astronomy. The central question — "Are we alone
Q_3_16 — Cosmochemistry: Meteorite Analysis, Presolar Grains, and Solar Composition
Cosmochemistry is the study of the chemical composition of the universe and the processes that produced it, with a primary focus on the analysis of meteorites — extraterrestrial rocks that survive passage through Earth's
INTERDOC_62 — Chemical Language Systems: Information Encoding from Microbes to Consciousness
Bacterial quorum sensing molecules encode population-density commands with combinatorial logic-gate precision (Bassler and Losick, 2006); microbial short-chain fatty acids (SCFAs) direct host immune programming, epigenet
Ocean_Climate_Civilization_Nexus
The relationship between ocean systems and human civilization is one of the most consequential and least integrated topics in historical analysis — most conventional histories treat the ocean as a static background, when
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