RESEARCH BASE

Search 3,721 documents across 34 fields — every claim tier-rated by evidence

3,721 Documents 34 Sections 43,625 Citations 34,852 Keywords Indexed 4 Evidence Tiers

3,633 are the core, quality-scored corpus (34 lettered sections — see How We Work); the remaining 88 are cross-corpus synthesis documents (68 InterDocs, 12 Connections, 8 Theories) also indexed here.

3,721 results for "salvinorin A" — page 79 of 187

ZB_5_23 Verified Ecology & Biology

ZB_5_23 — Bioacoustics & Animal Communication

Bioacoustics — the study of biological sound production, transmission, and reception — reveals a hidden world of communication systems of extraordinary sophistication. Humpback whale songs contain hierarchical structure

bioacoustics animal communication whale song birdsong echolocation soundscape ecology
ZB_4_16 Verified Ecology & Biology

ZB_4_16 — Mangrove Ecosystems

Mangroves are a group of approximately 70 species of salt-tolerant trees and shrubs that occupy the intertidal zone of tropical and subtropical coastlines worldwide, forming dense tidal forests that rank among the most p

mangrove blue carbon coastal wetland Rhizophora Avicennia carbon sequestration
ZB_4_07 Credible Ecology & Biology

ZB_4_07 — Deep-Time Ecology: Ecosystems across Geological History

Deep-time ecology reconstructs the structure, function, and dynamics of ecosystems over geological time — from the earliest microbial mats of the Archean (>3.5 Ga) through the emergence of complex life in the Ediacaran-C

deep-time ecology paleoecology fossil ecosystems Cambrian explosion reef evolution terrestrialization
ZB_4_10 Verified Ecology & Biology

ZB_4_10 — Cave Ecology: Life in Perpetual Darkness

Cave ecology (speleobiology) investigates life in subterranean environments — caves, groundwater aquifers, lava tubes, and interstitial spaces — habitats characterized by permanent darkness, near-constant temperature, hi

cave ecology speleobiology troglobite stygobite troglobite adaptations chemolithoautotrophy
ZB_4_11 Verified Ecology & Biology

ZB_4_11 — Island Ecology: Biogeography, Endemism, and Evolutionary Radiation

Island ecology — centered on the theory of island biogeography developed by Robert MacArthur and Edward O. Wilson (1963, 1967) — provides one of ecology's most influential theoretical frameworks, explaining how species d

island biogeography MacArthur-Wilson species-area relationship adaptive radiation endemism endemic species
ZB_4_08 Verified Ecology & Biology

ZB_4_08 — Rewilding and Ecological Restoration

Rewilding is an emerging approach to conservation that aims to restore self-sustaining, self-regulating ecosystems by reintroducing missing species — particularly large vertebrates and ecological engineers — and allowing

rewilding ecological restoration trophic rewilding Pleistocene rewilding ecosystem recovery reintroduction
ZB_4_09 Verified Ecology & Biology

ZB_4_09 — Canopy Ecology: Life in the Forest Roof

The forest canopy — the aggregate of tree crowns forming the uppermost vegetative layer of a forest — is among the most species-rich, least explored, and most ecologically dynamic habitats on Earth, harboring an estimate

canopy ecology forest canopy epiphyte arboreal vertical stratification emergent layer
ZB_4_02 Verified Ecology & Biology

ZB_4_02 — Extremophiles and Extreme Biology

Extremophiles are organisms that thrive in conditions lethal to most life — extreme heat, cold, acidity, radiation, pressure, salinity, or desiccation. Their discovery has fundamentally expanded understanding of life's b

extremophiles thermophiles halophiles acidophiles psychrophiles radiation resistance
ZB_4_14 Credible Ecology & Biology

ZB_4_14 — Acoustic Ecology: Soundscape Science and Biophonic Monitoring

Acoustic ecology — the study of the relationship between living organisms and their sonic environment — has evolved from an artistic and philosophical discipline into a quantitative ecological science with major conserva

acoustic ecology soundscape biophony Bernie Krause ecoacoustics noise pollution
ZB_4_06 Verified Ecology & Biology

ZB_4_06 — Alpine and Arctic Ecology: Life at the Extremes

Alpine and Arctic ecosystems — the treeless biomes occurring above the climatic treeline in mountains (alpine) and above ~60–70°N latitude where mean temperature of the warmest month is <10°C (arctic) — share fundamental

alpine ecology arctic ecology tundra permafrost treeline cryosphere
ZB_4_15 Credible Ecology & Biology

ZB_4_15 — Urban Wildlife Genomics: Rapid Evolution in the Anthropocene City

Cities — covering only ~3% of Earth's land surface but housing >55% of humanity — are emerging as powerful natural laboratories for studying rapid evolution in real time. Urban wildlife genomics investigates how the extr

urban-evolution wildlife-genomics urban-adaptation heat-island pollution-adaptation urban-speciation
ZB_4_03 Verified Ecology & Biology

ZB_4_03 — Desert Biology and Xerophytes

Deserts — regions receiving <250 mm of annual precipitation — cover ~33% of Earth's land surface and harbor organisms with some of the most remarkable adaptations in biology. Desert organisms face extreme challenges: wat

desert ecology xerophyte arid adaptation CAM photosynthesis water conservation succulent
ZB_4_05 Verified Ecology & Biology

ZB_4_05 — Urban Ecology: Nature in the City

Urban ecology studies the distribution, abundance, and interactions of organisms within cities and urbanized landscapes — environments that now house over 56% of humanity (projected ~68% by 2050) and cover ~3% of Earth's

urban ecology urban heat island habitat fragmentation synurbization novel ecosystems urban biodiversity
ZB_4_12 Verified Ecology & Biology

ZB_4_12 — Landscape Ecology: Patches, Corridors, and Mosaics

Landscape ecology studies how spatial patterns of ecosystems — the arrangement, size, shape, and connectivity of habitat patches within a heterogeneous landscape mosaic — influence ecological processes including species

landscape ecology patch dynamics connectivity corridor fragmentation metapopulation
ZB_4_13 Verified Ecology & Biology

ZB_4_13 — Historical Ecology: Human-Ecosystem Co-Evolution through Time

Historical ecology investigates how human land use, management, domestication, exploitation, and settlement over centuries to millennia have shaped contemporary ecosystems, landscapes, and biodiversity patterns — reveali

historical ecology shifting baseline land-use history legacy effects paleoecology human impact
ZB_3_22 Verified Ecology & Biology

ZB_3_22 — Old-Growth Forests & Ancient Woodland Ecology

Old-growth forests — variously defined as primary forests that have developed over centuries without major anthropogenic disturbance — represent the most structurally complex and biologically diverse terrestrial ecosyste

old-growth forest ancient woodland primary forest carbon sink biodiversity mycorrhizal network
ZB_3_14 Verified Ecology & Biology

ZB_3_14 — Kelp Forests and Seagrass Meadows: Underwater Gardens of Productivity

Kelp forests and seagrass meadows are the two major groups of marine macrophyte-dominated ecosystems — structurally complex, highly productive underwater habitats that provide essential services including nursery habitat

kelp forest seagrass macroalgae blue carbon urchin barren trophic cascade
ZB_3_23 Verified Ecology & Biology

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

coral reef bleaching zooxanthellae symbiosis ocean acidification Great Barrier Reef
ZB_3_07 Verified Ecology & Biology

ZB_3_07 — Keystone Species and Trophic Cascades

A keystone species exerts an ecological influence disproportionate to its abundance — its removal causes cascading structural changes through the ecosystem. The concept was introduced by Robert Paine (1966, 1969) based o

keystone species trophic cascade top-down regulation food web apex predator ecological engineer
ZB_3_19 Verified Ecology & Biology

ZB_3_19 — Permafrost Methane

Permafrost — permanently frozen ground maintained at or below 0°C for at least two consecutive years — underlies approximately 22% of the Northern Hemisphere land surface (about 23 million km²), primarily across Siberia,

permafrost methane thermokarst clathrate greenhouse gas Arctic warming