OXYGEN TRANSPORT
Oxygen Carrying Capacity
*The lowest value for fish is from the Antarctic Icefish which has no respiratory pigments and no red blood cells. The loss of resp. pigment is an adaptation in this fish that lives in cold, well-oxygenated waters. This fish also has a low metabolic rate (and activity levels, MR = _ to _ of allometric predictions) and enormous gill surface area, so oxygen dissolved in plasma is sufficient to meet its metabolic demands.
2) Chlorocruorins = greenish Hb, minor differences in porphyrin, otherwise identical to
Sipunculid worms, Priapulids, some polychaetes, at least one brachiopod (clam-like
bivalves).
molluscs and crustaceans.
Bohr Effect = rightward shift resulting from decreased pH (or increased carbon dioxide); Bohr Coefficient (ø) = D log P50/D pH; Magnitude of Bohr Effect increases with increasing Hb concentration, increasing temperature, and/or increasing ionic strength of plasma.
Root Effect = extreme rightward shift resulting from increased carbon dioxide or decreased pH; results in incomplete saturation at high pO2. Appears to be an exaggerrated Bohr effect; occurs in teleosts and some herps. Plays an important role in secretion of oxygen into swim bladder in teleosts.
4) Organic Phosphates and Other Modulators Organophosphate compounds and inorganic
ions inside RBC bind to Hb to modify conformation of oxygen affinity. Generally increased conc. of modulator causes a rightward shift.
increases oxygen carrying capacity (O2Cap).
C. Diving
1. No adjustment of oxygen affinity
2. No clear relationship between diving and P50 or diving and magnitude of Bohr effect.
3. Metabolic support of diving:
a) Short Dives - primarily aerobically supported
b) Long Dives - primarily anaerobically supported and often accompanied by a
reduction in total metabolism (See Overhead).
4. Primary Oxygen Stores during Dive:
b) In blood and tissues - high affinity Hb disadvantageous, enhanced Bohr effect advantageous.
(i) Most work has been done on whales and seals.
(ii) Generally higher oxygen carrying capacity in divers than in terrestrial
D. Development - proceeds in a specialized microenvironment that is potentially hypoxic (e.g., outer layers of egg present significant diffusion barrier, uterine environment in mammals less well oxygenated than maternal tissues).
1. Fish - Many show decrease affinity and decreased temperature sensitivity as development proceeds. SEE OVERHEAD.
2. Amphibians - Decreased oxygen affinity and increased sensitivity to acid on metamorphosis from tadpole to adult. Changes due to replacement of larval Hb with adult
Hb having a lower oxygen affinity. High affinity and low Bohr effect are adaptive in stagnant ponds (low O2 and potentially high CO2) where tadpoles live. SEE HANDOUT.
3. Reptiles - Decreased O2 affinity throughout development, apparently involves
increased organic phosphate levels within RBC.
4. Birds - Complex pattern of changing oxygen affinity throughout development. Initial increase
in affinity leading to a plateau at high affinity, affinity decreases prior to hatching. SEE HANDOUT.
- Changing oxygen affinity related to changing concentrations and types of organic phosphates (ATP early, DPG later in development, IPP in adult), and replacement of embryonic Hb types with adult Hb.
age may allow increased O2 extraction from hypoxic env. of egg, decreased affinity just prior to hatching may be related to exposure of embryo to ambient air.
5. Mammals - High oxygen affinity fetal blood, low oxygen affinity adult blood. Allows loading
of oxygen from maternal to fetal blood. SEE HANDOUT.
- Differences in affinity associated with:
a) Different types of Hb
(i) Ruminants show fetal Hb with intrinsically lower P50.
(ii) Primates have fetal Hb that is less responsive to DPG, and therefore has a higher affinity.
b) No structural difference, but increased levels of DPG in adults (dog, horse, mouse, opossum, etc.).
CO2 TRANSPORT IN BLOOD
I. Carried largely in chemical combination rather than as free dissolved CO2 (although CO2 much more soluble in aqueous solutions than oxygen).
A. Bicarbonate Ions - 80 to 90% of CO2 in venous blood.
CO2 + H2O ® H2CO3 ® H+ + HCO3-
1. The vast majority of CO2 from tissues diffuses through plasma into RBC.
2. Carbonic Anhydrase in RBC catalyzes conversions of:
CO2 + H2O ® H+ + HCO3-
- So that reaction proceeds rapidly to the right (rapid conversion impt. so that Bohr effect can enhance tissue unloading).
3. Build up of bicarbonate ions within RBC causes diffusion of bicarbonate ions into plasma; Chloride ions diffuse in from plasma to balance charges = Chloride Shift.
4. Most CO2 in the plasma is also carried as bicarbonate ions, but conversion is much slower.
B. Combined with Hemoglobin - CO2 binds to terminal amino groups on globin molecules, not to oxygen binding site. SEE HANDOUT FOR REVIEW.
of CO2 dissolved in water at normal partial pressures (40-45 torr for mammals).
SEE HANDOUTS FOR CO2 DISSOCIATION CURVES.
II. CO2 RELEASE (from blood to respiratory medium)
1. Assume RQ = 1.0 (O2 taken in = CO2 released).
2. Air
150 torr O2 ® 100 torr O2
Inspire Expire
0.2 torr CO2 ® 50.2 torr CO2
3. Water
150 torr O2 ® 100 torr O2
Inspire Expire
0.2 torr CO2 ® 3 torr CO2
- Difference in CO2 concentration on expiration is due to high solubility of CO2 in water.
4. Therfore, it is much easier to dump CO2 to environment for water-breathers than it is for air-breathers because the gradient is much steeper. SEE HANDOUT.
5. Aquatic organisms also capable of actively eliminating HCO3- through gill epithelium. SEE HANDOUT.
6. Since aquatic organisms can more easily eliminate CO2, they tend to have much lower blood pCO2 than terrestrial vertebrates (therefore blood buffering capacity lower and they are more sensitive to changes in pCO2).
III. BLOOD BUFFERS
a) Carbonic Acid - Bicarbonate System - (H+ + HCO3-)
b) Blood Proteins - Hb, plasma proteins
c) Phosphates - modifiers of oxygen affinity
4. Fish that deal with hypoxia regularly often show increased blood buffering capacities relative to normoxic fishes.
CO2 has less effect on elevating lethal pO2 in fishes which inhabit warm,
somtimes stagnant water.