Premed · Premed · General Biology 2

Lecture 14: Vertebrate Evolution

General Biology II — Organismal, Evolution & Ecology


Learning Objectives

By the end of this lecture, students will be able to:

  1. Describe the defining characteristics of chordates and the key features of vertebrates
  2. Outline the evolutionary history of vertebrates from jawless fish to mammals
  3. Compare the major vertebrate classes and their distinguishing adaptations
  4. Explain the key evolutionary transitions: evolution of jaws, transition to land, and evolution of the amniotic egg
  5. Describe the major adaptations that distinguish mammals and the radiation of mammalian orders
  6. Explain the evolutionary relationships among primates and the fossil record of human evolution

Lecture Content

I. Phylum Chordata: Defining Features

All chordates share four key features at some point during their development. The notochord is a flexible rod that provides structural support; in vertebrates, it is replaced by the vertebral column during embryonic development. The dorsal hollow nerve cord develops into the brain and spinal cord. Pharyngeal slits or clefts are openings in the pharynx that become gills in aquatic vertebrates and are modified into other structures in terrestrial forms, including the bones of the middle ear and the tonsils. The post-anal tail is a muscular extension past the anus that is reduced or vestigial in some species -- the human coccyx is its remnant.

The phylum includes three subphyla. Urochordata (tunicates or sea squirts) are marine animals whose free-swimming larvae display all four chordate features, but whose sessile, filter-feeding adults retain only the pharyngeal slits. Cephalochordata (lancelets, genus Branchiostoma) are small, fish-like marine organisms that retain all four chordate features as adults and serve as important models for understanding vertebrate origins. Vertebrata encompasses the animals that possess a vertebral column (backbone), a cranium (skull), and a highly developed brain.

II. Early Vertebrates: Jawless and Jawed Fishes

The earliest vertebrates were jawless fishes that appeared in the late Cambrian, approximately 530 million years ago. Among these were the conodonts (now extinct, known primarily from their tooth-like elements) and the ostracoderms (extinct armored jawless fishes). Two groups of jawless fishes survive today. Hagfish (Myxini) are marine scavengers that produce copious slime and possess only a cartilaginous skull without a true vertebral column. Lampreys (Petromyzontidae) include parasitic species that attach to fish hosts with a rasping mouth; they have a cartilaginous skeleton and a larval form that resembles the lancelet, hinting at deep evolutionary connections.

The evolution of jaws ranks among the most important innovations in vertebrate history. Jaws evolved from the modification of the anterior gill arches (pharyngeal arches), transforming passive filter feeders into active predators capable of exploiting entirely new food sources. This innovation triggered an adaptive radiation that produced the extraordinary diversity of jawed vertebrates (Gnathostomata) we see today.

Among the jawed fishes, the Chondrichthyes (cartilaginous fishes -- sharks, rays, skates, and chimaeras) retain a skeleton made entirely of cartilage. They bear placoid scales (tooth-like dermal denticles), continuously replace their teeth, lack a swim bladder (most must keep swimming to avoid sinking), detect water pressure changes through a lateral line system, and sense electric fields through the ampullae of Lorenzini. The Osteichthyes (bony fishes) are the most diverse vertebrate group, with approximately 30,000 species. The Actinopterygii (ray-finned fishes) constitute the vast majority, with fins supported by thin, flexible rays and a swim bladder for buoyancy control. The Sarcopterygii (lobe-finned fishes) have fins with a muscular base supported by bones -- a feature that foreshadowed the limbs of terrestrial vertebrates. The coelacanth (Latimeria), thought extinct until its discovery in 1938, and the lungfishes (Dipnoi), which can breathe air, are the closest living fish relatives of the tetrapods.

<image>A phylogenetic tree of major vertebrate groups. The tree shows the evolutionary relationships from the base: jawless fishes (lampreys, hagfish) branching off first, then the jawed fishes diverge into cartilaginous fishes (sharks, rays) and bony fishes. Bony fishes split into ray-finned fishes and lobe-finned fishes. From lobe-finned fishes, the tetrapod lineage emerges, branching into amphibians, then the amniote lineage which splits into reptiles (including birds) and mammals. Key evolutionary innovations are labeled at their branch points: vertebral column, jaws, bony skeleton, lungs/lobed fins, four limbs, amniotic egg, and hair/mammary glands. Representative organisms are drawn at each tip.</image>

III. The Transition to Land: Amphibians

Tetrapods -- four-limbed vertebrates -- evolved from lobe-finned fishes approximately 375 million years ago. The transitional fossil Tiktaalik, discovered in 2004, beautifully captures this transition: it possessed a fish-like body with scales and fins but also displayed tetrapod features including a flat head, a neck that could move independently of the body, and wrist-like structures in its pectoral fins that could support weight. Tiktaalik could likely prop itself up and move briefly on land.

Amphibians (frogs, salamanders, and caecilians, approximately 8,000 species) remain tied to moist environments by several features. Their skin is moist and permeable, serving as a major surface for gas exchange (cutaneous respiration) but also making them susceptible to desiccation. Most species have aquatic larvae (such as the tadpole) that undergo metamorphosis into terrestrial adults. Fertilization is typically external, with eggs laid in water. Amphibians are ectothermic, regulating their body temperature through behavior rather than internal heat production. Their three-chambered heart (two atria and one ventricle) allows some mixing of oxygenated and deoxygenated blood. The three living orders are the Anura (frogs and toads, the largest order), Urodela or Caudata (salamanders and newts), and Apoda or Gymnophiona (caecilians -- limbless, burrowing tropical amphibians). Amphibians are currently experiencing severe global declines driven by habitat loss, chytridiomycosis (the Bd fungal disease), climate change, and pollution.

IV. Amniotes: Reptiles, Birds, and Mammals

The amniotic egg was the key innovation that freed vertebrates from dependence on water for reproduction. The egg contains four extraembryonic membranes: the amnion, a fluid-filled sac that surrounds and cushions the embryo; the chorion, the outermost membrane involved in gas exchange; the allantois, which stores metabolic waste and participates in gas exchange; and the yolk sac, which provides nourishment. A shell -- leathery or calcified -- prevents desiccation. In placental mammals, these membranes have been repurposed for internal development, with the chorion and allantois contributing to the placenta.

A. Non-Avian Reptiles

Reptiles possess dry, scaly skin made of keratin that provides waterproofing and reduces water loss -- a dramatic improvement over the permeable amphibian skin. Most are ectothermic, employ internal fertilization, and lay amniotic eggs on land (or retain them internally). Their lungs are more efficient than those of amphibians, and they do not rely on cutaneous respiration. Most reptiles have a three-chambered heart, though crocodilians have evolved a four-chambered heart independently from birds and mammals. The major living groups include Testudines (turtles and tortoises), Squamata (lizards and snakes -- the most diverse reptile group), Crocodilia (crocodiles, alligators, and gharials -- the closest living relatives of birds), and Rhynchocephalia (the tuatara, a single living species from New Zealand often described as a living fossil).

B. Birds (Class Aves)

Birds evolved from theropod dinosaurs approximately 150 million years ago, with Archaeopteryx standing as the most famous transitional fossil. Every major feature of birds reflects adaptation for flight. Feathers, which are modified scales, provide both insulation and aerodynamic surfaces. Hollow, pneumatized bones reduce weight without sacrificing strength. A keeled sternum provides a large surface for the attachment of powerful flight muscles. Birds are endothermic, maintaining high body temperatures through an elevated metabolic rate. Their four-chambered heart completely separates oxygenated and deoxygenated blood, and their respiratory system features a unique unidirectional airflow through the lungs, supplemented by air sacs, that is more efficient than the tidal breathing of mammals. Birds excrete nitrogenous waste as uric acid (a paste rather than liquid urine) and lack a urinary bladder, both adaptations that reduce weight. With approximately 10,000 species, birds display remarkable diversity in beak shapes, feeding strategies, and habitats.

C. Mammals (Class Mammalia)

Mammals are defined by several key features. Hair or fur provides insulation and, in the case of whiskers, sensory input. Mammary glands produce milk to nourish young, a feature unique among vertebrates. Mammals are endothermic, maintaining constant body temperature through high metabolic rates. Their four-chambered heart ensures efficient oxygen delivery. A diaphragm -- a muscular sheet separating the thoracic and abdominal cavities -- aids breathing. Differentiated teeth (heterodonty) with distinct incisors, canines, premolars, and molars allow dietary specialization. A large, complex brain with an expanded neocortex supports advanced behavior, learning, and cognition. Three middle ear bones (malleus, incus, and stapes), derived from bones that were part of the reptilian jaw, provide exceptional hearing sensitivity.

The three major mammalian groups represent different reproductive strategies. Monotremes (platypus and echidnas) lay eggs but produce milk, though they lack nipples. Marsupials (kangaroos, koalas, opossums) give birth to highly undeveloped young that complete their development in a pouch (marsupium). Eutherians (placental mammals) undergo extended gestation with nourishment provided through a placenta, producing relatively well-developed offspring. Placental mammals, with approximately 5,000 species, are by far the most diverse group. Mammals originated approximately 220 million years ago but remained small throughout the age of dinosaurs. After the end-Cretaceous mass extinction 66 million years ago, mammals diversified rapidly into the ecological niches vacated by the dinosaurs, producing the major orders we know today: Rodentia (the most species-rich), Chiroptera (bats), Carnivora, Primates, and Cetartiodactyla (whales and even-toed ungulates).

<image>A diagram illustrating the amniotic egg and its extraembryonic membranes. Panel A: Cross-section of a reptilian/bird shelled egg showing the embryo at the center surrounded by the amnion (filled with amniotic fluid). The yolk sac is connected to the embryo ventrally, providing nutrients. The allantois is shown as a sac collecting metabolic waste and participating in gas exchange. The chorion is the outermost membrane, lining the inside of the shell. The shell and shell membrane are labeled on the exterior. Arrows indicate gas exchange (O2 in, CO2 out) across the shell and chorion/allantois. Panel B: A comparison showing the mammalian (placental) equivalent — the chorion and allantois contribute to the placenta, which interfaces with the uterine wall; the amnion surrounds the fetus; the yolk sac is vestigial. Labels identify each membrane in both panels.</image>

V. Human Evolution

Primates are characterized by grasping hands with opposable thumbs, forward-facing eyes providing binocular vision, large brains relative to body size, and extended parental care. Within the primates, the Hominoidea (apes) -- gibbons, orangutans, gorillas, chimpanzees, and humans -- are distinguished by the absence of a tail. The Hominini (hominins) includes humans and their extinct ancestors after the evolutionary split from the chimpanzee lineage, approximately 6-7 million years ago.

The hominin fossil record reveals a progression of increasingly human-like forms. Sahelanthropus tchadensis (approximately 7 Ma) is among the earliest known hominins. Ardipithecus ramidus (approximately 4.4 Ma) was a facultative biped. Australopithecus afarensis, represented by the famous "Lucy" skeleton at approximately 3.2 Ma, was clearly bipedal but retained a small brain of about 400 cc. Homo habilis (approximately 2.4 Ma), the "handy man," used stone tools and had a brain of about 600 cc. Homo erectus (approximately 1.9 Ma to 110 Ka) had a substantially larger brain of about 900 cc, used fire, and was the first hominin to migrate out of Africa. Homo neanderthalensis (approximately 400 to 40 Ka) possessed a large brain of approximately 1,400 cc, was adapted to cold European climates, and -- as genomic evidence has revealed -- interbred with Homo sapiens, contributing 1-4% of the DNA in modern non-African human populations. Homo sapiens appeared approximately 300 Ka with a brain of about 1,350 cc and the capacity for language, culture, and sophisticated technology.

Several key trends characterize human evolution. Bipedalism evolved early, well before the dramatic brain enlargement that followed. Brain size increased substantially over hominin evolution. Jaw and tooth size decreased as diet changed and food processing became more sophisticated. Tool use progressed from simple stone flakes to increasingly complex technologies. And multiple waves of migration carried hominin populations out of Africa and across the globe.


Lecture 14: Vertebrate Evolution — figure 1
Lecture 14: Vertebrate Evolution — figure 2

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