Mountain climbers struggling to breathe astride the 29,029 foot (8,848 meter) summit of Mt. Everest routinely see birds gracefully flying above them, engaging in nonchalant aerial acrobatics at altitudes where humans risk hypoxia (oxygen starvation) while standing still.
The avian respiratory system is at least 33% more efficient than any mammalian lung. Birds combine lungs with an extensive system of air sacs - permitting a unidirectional airflow of 'fresh' air with a higher oxygen content. Mammals are saddled with bidirectional lungs that mix 'fresh' and 'stale' (carbon dioxide-laden) air.
Since birds descended from dinosaurs - they are avian dinosaurs - what does this say about dinosaurian respiration, the world in which they evolved, and more specifically the atmospheric chemistry of the planet they came to dominate?
"Out of Thin Air: Dinosaurs, Birds, and Earth's Ancient Atmosphere" by Peter Ward hypothesizes that the history of atmospheric and oceanic oxygen levels throughout geologic time has profoundly impacted the nature of animal life on Earth - everything from morphology (body plans) and physiology to evolutionary history and diversity - was contingent on oxygen levels which have varied radically over time.
Ward, a paleontology professor at the University of Washington, and a NASA staff astrobiologist, is an expert in paleo-atmospheric chemistry and supports his claims with ample and compelling evidence.
Earth's atmosphere presently consists of 78% nitrogen and 21% oxygen, the final 1% composed of various gases; carbon dioxide being the most notable and problematic. 4.54 billion years ago Earth's atmosphere was a hothouse dominated by carbon dioxide. Oxygen was so scarce that Iron could not rust. Photosynthetic cyanobacteria introduced oxygen into Earth's atmosphere - precipitating an oxygen crisis - the first known mass extinction.
Since the advent of photosynthesis atmospheric oxygen levels hare varied considerably. Only 5 million years ago (MYA) oxygen levels hit 28%. The early Cambrian (544 MYA) averaged 13% and levels peaked during the Carboniferous - Permian transition (299 MYA) at 35%. By the Permian - Triassic boundary (251 MYA) oxygen levels plummeted to less than 12%.
Mass extinctions periodically reshape life on Earth. The best known, the Cretaceous - Tertiary (K-T) boundary, ended the reign of the non-avian dinosaurs approximately 65 MYA when an asteroid roughly 10 kilometers wide gouged the Chicxulub crater near the Yucatan Peninsula, setting the stage for mammals, including Homo sapiens, to become the dominant terrestrial vertebrates.
Another extinction event, the Permian - Triassic (P-Tr), some 251 MYA, is informally known as 'the Great Dying.' Up to 96 percent of all marine species and 70 percent of terrestrial species were erased as global ecosystems crumbled. Life itself nearly died as a greenhouse gas spike caused temperatures to soar 10 - 30 degrees Celsius (18 - 54 degrees Fahrenheit), and oxygen levels plummeted when the oceans became the anoxic (without-oxygen) abode of methanogenic and sulfate-reducing microorganisms - amplifying global warming (methane is 10 times more efficient than carbon dioxide at trapping heat in the atmosphere) and poisoning plant and animal life with deadly hydrogen sulfide (rotten egg gas). The sky literally turned a sickly shade of green, a topic ably covered in Ward's superb Under a Green Sky: Global Warming, the Mass Extinctions of the Past, and What They Can Tell Us About Our Future.
Since dinosaurs evolved in the early Triassic - a period of suffocatingly low (to mammals) oxygen levels - any evolutionary innovations that enhanced respiratory efficiency would provide a compelling advantage. Ward contends that dinosaurs eclipsed the dominant Therapsida (mammal-like reptiles) and early mammals by evolving the unidirectional airflow lung and air sack respiratory system utilized by their avian descendents. In the Cynognathus vs. Eoraptor world of the early Triassic the race was to the swift and battle to the strong - our ancestors lost. Therapsids went extinct, early mammals retreated to niches where their respiratory and metabolic systems could cope with Triassic atmospheric conditions, and the reign of the dinosaurs began.
Along the way Ward lucidly engages a wide array of topics to make his case. The impact of continental drift (plate tectonics) and geochemistry (sulfur and carbon cycles) on oxygen levels are explored. Segmented body plans as a respiratory strategy, gills (trilobite, cephalopod, and decapod), and lungs of every variety (from alveolar to septate) are contrasted. The advent of endothermy (warm-blooded metabolism), evidence for same (turbinal bones in mammal-like reptiles and early mammals), and associated reproductive strategies (eggs vs. live birth) also illuminate Ward's insights. Circulatory advances (four-chamber hearts), even the upright posture of dinosaurs (Ward suggests the need to breathe while walking drove this innovation) are deftly dropped into a compelling evidentiary mosaic.
"Out of Thin Air" is more than a trendy title - the science shows how the dinosaurs literally emerged as a result of 'thin' air due to near-hypoxic atmospheric oxygen levels prevailing throughout the P-Tr transition. Dinosaur enthusiasts will be enthralled and mystery lovers will applaud Ward's 'science as the ultimate sleuth' approach to deciphering the history of life on Earth. Ward's Gorgon: The Monsters That Ruled the Planet Before Dinosaurs and How They Died in the Greatest Catastrophe in Earth's History makes an excellent companion volume.