Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Dinosaur thermoregulation Were they “warm blooded”?
Thermogram of a lion Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Body temperature in endotherms and ectotherms
Thermogram of ostriches Thermogram of a snake wrapped around a human arm
Thermogram of a python held by people Thermogram of a lion Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Physiology, metabolism, and dinosaurs? Ornithopods Birds Sauropods Dromeosaurs Tyrannosaurus Ceratopsians Pachycephalosaurs Crocodilians Stegosaurs Ankylosaurs Lizards and snakes Lizards
? ? ? ? ? ? ? Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
“extant phylogenetic bracket”
Using phylogenetic logic to reconstruct biology of extinct animals.
Features observed in living animals can be traced back to common ancestor. This suggests that extinct clades that fall between are likely to have similar in features even if they cannot be observed directly in the fossils.
Witmer, 1995 Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Thermoregulation
Maintaining body temperature within limited boundaries regardless of temperature of the surrounding environment.
Endotherm vs. Ectotherm
Endotherms use internal metabolic heat to regulate themselves, ectotherms use external sources of heat (and cool). Mammals and birds are endotherms, most other vertebrates are ectotherms.
Homeotherm vs. Poikilotherm
Homeotherms have a constant body temperature, poikilotherms have a variable body temperature. Mammals are homeotherms, but so are fish that live in water of constant body temperature. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Endothermic groups In-between groups Mammalia (mammals) Very large animals (inertial Aves (birds) homeotherms) Animals with unusual physiology (tuna are endothermic)
Unknown groups Ecothermic groups Non-avian dinosaurs most fishes Amphibia Pelycosaurs (non-mammalian synapsids) Lepidosauria (lizards and snakes) Crocodilians Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Source of internal heat
Anaerobic metabolism Produces lactic acid Less energy stored in ATP
Aerobic metabolism
Produces carbon dioxide Stores more energy in ATP Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Duration of energy output in ectotherms and endotherms Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Mechanisms for regulating body temperature
Regulate production of heat by changing metabolism • shivering • torpor Regulate amount of blood at surface of body • “counter current” exchange (arteries and veins intertwine in legs and other places so that outgoing blood is cooled by returning blood and vice versa) • dilation and constriction of blood vessels (blushing, shock) Insulation • hair • feathers • subcutaneous fat Evaporative cooling • sweating • panting Behavioral regulation • sunning • moving into shade • denning • lying on cool mud or in water • Expose wing surfaces Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Behavioral thermoregulation in an ectotherm
From Shine, 1991, Australian Snakes, A Natural History, Cornell. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Changes in body temperature in ectothermic poikilotherm
95F
From Shine, 1991, Australian Snakes, A Natural History, Cornell. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Poikilotherm and variation in body temperature Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Inertial homeothermy probable in large dinosaurs
Large animals retain heat because their surface area is proportionally smaller.
An inertial homeotherm is an ectotherm that is so large that it cannot exchange heat across the surface fast enough to keep up with changing environment temperature. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Metabolic rate is related to body size in ectotherms (mammals)
1.50 /hr/g)
2 1.00
0.50
0.00
-0.50
-1.00
Logmetabolic rate(O -1.50 -4.0 -2.0 0.0 2.0 4.0
Log body mass (kg) Data from Eisenberg, 1981 Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Vertebrate dietary categories
Omnivore - mixed diet
Frugivore - diet Herbivore - generalized specializing on fruits (only diet on plant leaves and exists after the stems Cretaceous)
Granivore - diet Piscivore - carnivorous diet specializing on seeds and specializing on fish nuts
Insectivore - diet specializing on insects (and sometimes other Carnivore - generalized diet invertebrates, like of flesh and fat worms) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Energy value in different food sources
Small ectotherms = high metabolic rate = high calorie diet = small animals must be insectivores and granivores Large ectotherms = lower metabolic rate = lower calorie diet = large animals can be herbivores and frugivores
700
525
350 kcal per 100 g
175
0 Insects Nuts and Seeds Meat and Fat Fruits Leaves and Grasses Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Skeletal evidence for conserving heat
Turbinal bones Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Deterministic growth and physiology
Deterministic growth: rapid growth to fixed adult size (birds and mammals)
Indeterminate growth: slower growth with no maximum size
Growth patterns are related to endothermy Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Deterministic growth in dinosaurs Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Rates of growth in dinosaurs Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Structure of mammalian bone Haversian system - blood vessels nourish osteocytes, chondrocytes, and provide minerals for bone deposition in concentric rings around the vessels
Kardong 1995, Vertebrates Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Histology of fossil bone Osteons (or Haversian structures
Modern bone Jurassic age plesiosaur (Martill, 1991, Bones as stones) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Bone histology and the rate of growth in dinosaurs
Padian, Horner and de Ricqlès, 2004, J. Vert. Paleo, 24: 555-571. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Climate and ectotherms Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Titanoboa and temperature in the Paleogene Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
How big was Titanoboa?
Regression of SVL on vertebra width P < 0.001, R2 = 0.7
Total body length: 12.82 m +/- 2.18 m (42 ft) Body mass: 1,135 kg (1.27 tons)
Living anaconda: Record = 7 m, Average = 6.5 m An adult Ball python slithering over a Living python: Record = 9 m, Average = 6 m Titanoboa vertebra. (c) 2009, Jason J. Head
(Graphic by Brady MacDonald (c) 2009, LA Times)
Head, J.J., J.I. Bloch, A.K. Hastings, J.R. Bourque, E. Cadena, F. Herrera, P.D. Polly, and C.A. Jaramillo. 2009. Giant boine snake from a Paleocene Neotropical rainforest indicates hotter past equatorial temperatures. Nature, 457: 715-718. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Global Climate for the last 65 million years Present 14 C (57.2 F)
Last Glacial Maximum 9 C (48.2 F)
Miocene Climatic Optimum 21 C (70 F)
Eocene thermal maximum 23-26 C (73-79 F)
(Zachos et al., 2001. Science, 292: 686-693) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Titanoboa’s world
(Zachos et al., 2001. Science, 292: 686-693) (© 2010, Ron Blakey, NAU Geology) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Climate in the Paleogene circles = no frost intolerant plants squares = palms triangles = cycads, gingers or tree ferns
Eocene Metasequoia stumps, Axel Heiberg Island (photo by Greenwood)
(Greenwood & Wing, 1995. Geology, 23: 1044-148. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Why was Titanoboa so big? Size, metabolism and temperature in poikilotherms*
mass specific metabolism b is lower in larger organisms, placing limit on maximum size (B = base metabolic rate, M = body mass)
Max size (Lmax) is function of temperature and base metabolic rate Record sizes for living poikilotherms
Relative size is proportional to temperature
Makarieva, A.M, V.G. Gorshkov, and B-L. Li. 2005. Temperature- associated upper limits to body size in terrestrial poikilotherms. Oikos, 111: 425-436. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Reptile paleothermometer Estimated temperatures at Titanoboa site
Minimum MAT from Titanoboa : 32-33°C
Minimum MAT from giant fossil turtle: 32-33°C
dO18 from Forams: 28-31°C
fossil plants: 26-28°C (known underestimate)
Head, J.J., J.I. Bloch, A.K. Hastings, J.R. Bourque, E. Cadena, F. Herrera, P.D. Polly, and C.A. Jaramillo. 2009. Giant boine snake from a Paleocene Neotropical rainforest indicates hotter past equatorial temperatures. Nature, 457: 715-718. Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Other giant reptiles of the Paleocene Size evolution in relation to climate Palaeophis snake
Gigantophis snake
podocnemidid turtle
Agamid lizard Boid snake Drazindaretes turtle (Head et al., in prep) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114
Sea-surface temperature today
28°F 87°F
Middle Cretaceous 34°C - 42°C 93°F - 107°F