vertebrate physiology ecol 437 university of arizona fall

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Lecture 18, 30 Oct 2003 Chapter 12, Circulation (con’t) Chapter 13, Respiration, Gas Exchange, Acid-Base Balance Vertebrate Physiology ECOL 437 University of Arizona Fall 2003 instr: Kevin Bonine t.a.: Bret Pasch 1

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Page 1: Vertebrate Physiology ECOL 437 University of Arizona Fall

Lecture 18, 30 Oct 2003Chapter 12, Circulation (con’t)

Chapter 13, Respiration, Gas Exchange, Acid-Base Balance

Vertebrate PhysiologyECOL 437

University of ArizonaFall 2003

instr: Kevin Boninet.a.: Bret Pasch

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Page 2: Vertebrate Physiology ECOL 437 University of Arizona Fall

Vertebrate Physiology 437

1. Circulation (CH12)

2. Blood-Gas Chemistry (CH13)

3. Announcements...

2

14-34, Vander 2001

See (12-32)

Page 3: Vertebrate Physiology ECOL 437 University of Arizona Fall

Thursday, 30 October -- the ARLDN's 2003 Edmund A. ArbasLecturer, Prof. Peter M. Narins from the Dept. of Physiological Science atUCLA, will give his public lecture in Economics 110 at 4:00 pm. The titleof his lecture is "Science on Seven: Adventures of an ExpeditionaryBiologist."

Narins is renowned for his elegant work on hearing and auditorycommunication in frogs and is a world leader in neuroethology, animalbehavior, and auditory neurophysiology. He is also a legendary fieldbiologist, having led 39 expeditions to remote and exotic field sites onseven continents over the last quarter century. A masterfully clear andvery entertaining speaker, he has won the most prestigious teachingawards atUCLA.

2b

Page 4: Vertebrate Physiology ECOL 437 University of Arizona Fall

Name that student:

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Drew StasiakChem Minor

Elena CostinMCB

Gabriel ReinhardtMCB

Page 5: Vertebrate Physiology ECOL 437 University of Arizona Fall

Hemodynamics in Vessels

Vander 2001

14-11, Vander 2001

Flow depends primarily on pressure gradient and resistance

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Page 6: Vertebrate Physiology ECOL 437 University of Arizona Fall

Hemodynamics

- Poiseuille’s Law:

Flow rate

8Lη

Q = (P1 – P2)πr4

Pressure Gradient

radius4

length viscosity

Use to approximate flow

Small change in radius large change in flow rate

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Page 7: Vertebrate Physiology ECOL 437 University of Arizona Fall

Hemodynamics

- From Poiseuille’s Law:

Resistance

Q

R = (P1 – P2)

Pressure Gradient

radius4

Flow rate

viscosity

Small change in radius large change resistance

= 8Lη

πr4

length

Modifiable if vessel distensible under pressure

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Page 8: Vertebrate Physiology ECOL 437 University of Arizona Fall

(12-25)

Summed resistancereduces pressure…

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Page 9: Vertebrate Physiology ECOL 437 University of Arizona Fall

(12-23)

Total Flow Rate same allalong Circulatory System

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River

Lake

River

Page 10: Vertebrate Physiology ECOL 437 University of Arizona Fall

(12-24)

Shapes of curves slightly different because ofRBCs (viscosity) and fact that they tend to flowin middle of lumen

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Page 11: Vertebrate Physiology ECOL 437 University of Arizona Fall

Peripheral Circulation

- Endothelium lining vessels- Middle layer with smooth muscle (esp. arteries)- Outer fibrous layer

Capillaries with ~ only Endothelium

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Page 12: Vertebrate Physiology ECOL 437 University of Arizona Fall

(12-26)

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Page 13: Vertebrate Physiology ECOL 437 University of Arizona Fall

Peripheral Circulation

Compliance vs. Elasticity

~ Veins vs. Arteries

Volume Reservoir vs. Pressure Reservoir

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Page 14: Vertebrate Physiology ECOL 437 University of Arizona Fall

Volume Reservoir vs. Pressure Reservoir

14-34, Vander 2001

(12-27)~Constant P and Q at Capillaries!

See (12-32)

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Page 15: Vertebrate Physiology ECOL 437 University of Arizona Fall

Venous System

- low pressure (11 mm Hg or less)

- thin walled veins with less muscle

- more compliant and less elastic

- valves

- blood moved by skeletal muscle (and smooth)

- breathing creates vacuum (low pressure) inchest to aid blood flow to heart

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Page 16: Vertebrate Physiology ECOL 437 University of Arizona Fall

Microcirculation

- endothelium in capillaries is permeable

1. continuous

2. Fenestrated (kidney, gut)

3. Sinusoidal (liver, bone)

Less permeable

- Movement across walls, between walls, in vesicles

More permeable

- Bulk Flow…

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Page 17: Vertebrate Physiology ECOL 437 University of Arizona Fall

Bulk Flow…

Fluid Pressurevs.Osmotic Pressure

(12-38)

Filtration > Uptake

Lymph System to return excess fluid

Faster than diffusion

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Page 18: Vertebrate Physiology ECOL 437 University of Arizona Fall

Bulk Flow… - Edema

- No RBCs; therefore not red

Lymph System

- Starvation- Lungs- Kidneys

- Drains interstitial spaces- has valves and smooth musculature- empties into thoracic duct at vena cavae- transport system for large hormones and fats into blood stream- filariasis, elephantiasis- Reptiles and Amphibians with lymph hearts

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Page 19: Vertebrate Physiology ECOL 437 University of Arizona Fall

Giraffe example pgs. 504-505

Why does blood in the lowerextremities of aquatic organismsnot pool as it may do in legs of

humans, giraffes, etc.?

FISH:

Blood tends to pool in tail b/c inertia andcompression waves when swimming

-Veins in middle of body-Accessory caudal (tail) heart in some species

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Page 20: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

1. Feed Brain and Heart First2. Next Feed Tissues in Need3. Maintain volume, prevent edema, etc.

BaroreceptorsChemoreceptorsMechanoreceptorsThermoreceptors

Info. integrated at Medullary Cardiovascular Centermedulla oblongata and pons

Depressor Center Parasympathetic Effectors

Pressor Center Sympathetic Effectors

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Page 21: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Baroreceptors increase AP firing rate when BP increases

Sensed at carotid sinus,aortic arch, subclavian,common carotid,pulmonary

Usually leads to Sympatheticsuppression to decrease BP

(12-43)

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Page 22: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Arterial Chemoreceptors in carotid and aortic bodies(More details when discuss ventilation)

e.g., low O2, high CO2, low pHleads to bradycardia and peripheral vasoconstriction(diving and not inflating lungs)

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What about when not diving?

Page 23: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Cardiac Mechanoreceptors and Chemoreceptors

Alter heart rate AND blood volume

e.g.,ANP (Atrial Natruiretic Peptide) released in response to stretch

- leads to increased Na+ excretionand therefore greater urine output

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Page 24: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Extrinsic vs. Local Control

Neuronal orHormonal

Most arterioles with sympathetic innervation

Also respond to circulating catecholamines:

-At high levels, alpha adrenoreceptors are stimulated vasoconstriction (to increase BP)

-At low levels, beta2 adrenoreceptors are stimulated vasodilation (to increase flow to tissue)

-Response depends on tissue type, receptor type(s), levelof catecholamines (epi, norepi), etc.

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Page 25: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Extrinsic vs. Local Control

Neuronal orHormonal

Neuropeptide Y

- Acts by reducing IP3 levels

-decreases coronary blood flow-decreases heart contractility

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Page 26: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Extrinsic vs. Local Control

stretch

temp.O2CO2pHadenosineK+

Decreased O2 levels withopposite effect in lungs

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Page 27: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Extrinsic vs. Local Control

(12-45)

-Vasodilation-Relaxation

-Viagra acts by blockingbreakdown of cGMP

NO (nitric oxide)

Released fromvascular endothelium:

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Page 28: Vertebrate Physiology ECOL 437 University of Arizona Fall

Circulatory System Regulation

Extrinsic vs. Local Control

-Vasodilation

Histamine

Released in responseto injury of connectivetissue and leukocytes:

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Page 29: Vertebrate Physiology ECOL 437 University of Arizona Fall

Chapter 13

Gas exchangeAcid-base balance

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Page 30: Vertebrate Physiology ECOL 437 University of Arizona Fall

Gas composition in air O CO N

% of dry air 21 0.03 78

pp at 760 mm Hg 159 0.23 594

380mmHg (at 6000m) 79.6 0.11 297

Solubility in water (ml/L) 34 1,019 17

2 2 2

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End

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