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361 results for "contemporary evolution" — page 13 of 19
ZF_2_00 — Marine Biology Ecology: Subfolder Summary
ZF_2_12 — Deep-Sea Gigantism and Abyssal Ecology
Deep-sea gigantism (also called abyssal gigantism) is the observed tendency for certain deep-sea invertebrates and some vertebrates to attain body sizes far exceeding those of their shallow-water relatives — a pattern do
ZF_2_19 — Marine Bioluminescence: Light in the Deep Ocean
Bioluminescence — the production and emission of light by living organisms through chemical reactions — is the most widespread form of communication in the ocean and arguably the most common visible phenomenon on Earth,
ZF_2_10 — Sharks and Apex Marine Predators
Sharks — cartilaginous fishes of the superorder Selachimorpha (~500 living species) — are among the ocean's most ancient and ecologically critical predators, having evolved over 400 million years (predating trees and din
ZF_3_10 — Marine Paleontology and the Fossil Record of the Seas
Marine paleontology documents the evolution of life in Earth's oceans over ~3.8 billion years — from the earliest microbial fossils (stromatolites, ~3.5 Ga) to the complex marine ecosystems of the modern ocean. The marin
ZF_5_00 — Ocean Technology Policy: Subfolder Summary
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
ZF_0_00 — Oceanography & Marine Science: Section Summary
Z_5_08 — Mitochondrial DNA: Maternal Inheritance, Ancient Lineages, and Disease
Mitochondrial DNA (mtDNA) — the small, circular genome (~16,569 base pairs in humans) contained within mitochondria — encodes 37 genes essential for oxidative phosphorylation (13 protein-coding genes, 22 transfer RNAs, 2
Z_3_16 — Genomic Conflict and Selfish Genetic Elements
Selfish genetic elements (SGEs) — sequences of DNA that promote their own transmission at the expense of the host organism or other genes in the genome — reveal that the genome is not a cooperating community of genes but
Z_3_13 — Horizontal Gene Transfer in Prokaryotes
Horizontal gene transfer (HGT) — the movement of genetic material between organisms outside of parent-to-offspring inheritance — is a dominant force shaping prokaryotic evolution, fundamentally challenging the traditiona
Z_2_07 — Genetics of Disease Resistance
Infectious disease has been the most powerful selective force shaping the human genome, leaving signatures across thousands of loci. The best-understood example is sickle cell disease (HbS, Glu6Val in HBB): heterozygous
Z_1_00 — Genome Structure Organization: Subfolder Summary
Z_4_07 — The Tree of Life: Molecular Phylogenetics and Universal Ancestry
The Tree of Life — the branching diagram representing the evolutionary relationships among all living organisms — has been fundamentally reshaped by molecular phylogenetics, the reconstruction of evolutionary history usi
Z_0_00 — Molecular Biology & Genomics: Section Summary
K_3_00 — Consciousness Variants: Subfolder Summary
K_3_11 — Animal Consciousness and Sentience
The question of whether non-human animals possess conscious experience — subjective awareness, felt pain, emotions, and self-recognition — has moved from philosophical speculation to a major neuroscientific research prog
E_2_12 — Great Oxygenation Event
The Great Oxygenation Event (GOE) — approximately 2.4–2.1 billion years ago — was one of the most transformative events in Earth's history: the first permanent rise of free molecular oxygen (O₂) in the atmosphere, from n
E_2_11 — Snowball Earth Hypothesis
The Snowball Earth hypothesis proposes that Earth's surface was entirely or nearly entirely covered by ice on at least two occasions during the Neoproterozoic era (c. 720–635 million years ago): the Sturtian glaciation (
E_4_24 — Quaternary Science: Integrating Ice Ages, Extinctions, and Migrations
Quaternary science is the interdisciplinary study of Earth's most recent geological period — the Quaternary (2.58 Ma to present), encompassing the Pleistocene (2.58 Ma to 11,700 BP) and the Holocene (11,700 BP to present
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