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Responses of renal inner medullary collecting duct cells (IMCD) to osmotic stress. Maurice B. Burg NHLBI, Bethesda, MD 20897-1603, maurice_burg@nih.gov Accompanying urinary concentration and dilution, IMCD cells are exposed to concentrations of NaCl and urea that are variable and often very high (total $1700 mosm), yet the cells survive and function. Accumulation of compatible and counteracting organic osmolytes and activation of heat proteins were previously identified as important factors. We have been further investigating the mechanisms involved, using cultures of mouse IMCD cells that are either early passage or are immortalized with SV40 (mIMCD3). With mIMCD3 cells, a step increase in osmolality from 300 to a total of 500-600 mosm stops proliferation for ~18 h, followed by renewed growth at the original rate. Increase to ~700 mosm kills most cells by apoptosis. Elevating to 500-600 mosm with NaCl (but not with urea) causes DNA double strand breaks and activates p53, a tumor suppressor protein, causing the cell cycle delay. Suppression of p53 abrogates the cell cycle delay and cells that proceed to replicate damaged DNA become apoptotic. At ~700 mosm (but not at 500-600) there is rapid decrease in mitochondrial PD and exit of NADPH from the mitochondria followed by cell death. Early passage IMCD cells survive linear (over 18 hours, like in vivo), but not step, increases to ~1700 mosm. The difference presumably is that a step increase rapidly increases intracellular ionic strength, which damages DNA, whereas linear increase gives time for organic osmolytes to accumulate, minimizing intracellular ionic strength and DNA damage.
Volume regulation during dehydration of East-African desert beetles Karl Erik Zachariassen Department of Zoology, Norwegian University of Science and Technology (NTNU), 7491 Trondheim, Norway In arid areas in East Africa dietary water is not available during the
dry seasons. Since the dry seasons may last for many months, sometimes
for more than a year, insects living in these areas may become severely
dehydrated and in extreme cases lose more than 80% of their body water. Protective properties of organic osmolytes in deep-sea fish and vestimentiferans Paul H. Yancey, Wendy Blake, James Conley Biology Department, Whitman College, Walla Walla, WA 99362 USA, yancey@whitman.edu Hydrostatic pressure (1 atm per 10m depth) perturbs protein stability
and function; many proteins in deep-sea organisms have evolved resistance
to this, but many still retain sensitivity. Recently our laboratory has
found unusual osmolyte levels in deep-sea animals. Trimethylamine N-oxide
(TMAO), usually under 100 mmol/kg wet wt. in most shallow animals, increases
with depth in muscles of teleost fishes and decapod crustaceans, reaching
300 mmol/kg at 3000m. The giant vestimentiferan Riftia (from 2500m,
near hydrothermal vents) contains the unusual osmolyte hypotaurine at
125 mmol/kg. The animal experiences both high pressure and rapid temperature
changes from 5 to 25°C, which could perturb proteins. We tested our
hypothesis that these osmolytes counteract pressure and/or temperature
effects. With proteins from abyssal grenadier fish at 300-500 atm, 250
mM TMAO fully offset pressure inhibition of stability and cofactor binding
of lactate dehydrogenase and of actin polymerization actin. Glycine, a
common shallow-water osmolyte, was not protective. To test the universality
of TMAO protection, yeast were cultured, pressurized and plated. For 1
hr at 700 atm, 3.5 hr at 700 atm, and 17 hr at 300 atm, 150 mM TMAO generally
doubled the number of surviving cells. For Riftia malate dehydrogenase
incubated at 300 atm for 24 hr, 125 mM hypotaurine only partly offset
a 32% loss of activity at 5, but fully offset a 35% loss at 25°C,
thus showing greater protection at the higher temperature. Calcium homeostasis in crustaceans: evolutionary considerations Michele Wheatly and Flavia P. Zanotto Wright State University and University of Sao Paulo Calcium homeostasis in crustaceans is influenced by their natural molting
cycle that periodically requires replacement of the calcified exoskeleton
in order for growth to occur. Whole body Ca balance transitions from intermolt
(zero net flux) to premolt (net efflux) and postmolt (net influx at the
rate of 2 mmol/kg/h). As such, molting provides a convenient model to
study up- and down regulation of epithelial Ca transporting proteins (such
as Ca pumps and exchangers), the genes that encode them, and the steroid
hormone (ecdysone) that putatively regulates the genes. Species residing
in either fresh water or in terrestrial environments are more limited
in their Ca availability than are marine species. Further the advance
towards terrestriality is accompanied by decreased reliance upon branchial
Ca uptake and increased reliance upon digestive uptake. This plenary lecture
will correlate Ca handling strategies with environment in a range of species
through examining extracorporeal, extracellular and intracellular Ca compartments.
Methodological approaches will include systems physiology, epithelial
transport (gills, antennal gland, hepatopancreas and hypodermis), subcellular
homeostasis and molecular regulation. Flow cytometry and polyclonal antibodies
will be introduced as novel techniques to assist with the elusive stages
of pre- and postmolt.
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