Repeating earthquakes record fault weakening and healing in areas of megathrust postseismic slip.

Repeating earthquakes (REs) rupture the same fault patches at different times allowing temporal variations in the mechanical behavior of specific areas of the fault to be interrogated over the earthquake cycle. We study REs that reveal fault weakening after a large megathrust earthquake in Costa Rica, followed by fault recovery. We find shorter RE recurrence intervals and larger slip areas immediately following the mainshock that both gradually return to pre-earthquake values. RE seismic moments remain nearly constant throughout the earthquake cycle. This implies a balance between fault weakening (reducing slip) and transient embrittlement (increasing rupture area by converting regions from aseismic to seismic slip), induced by the increased loading rate following the mainshock. This interpretation is consistent with positive, negative, and constant moment versus RE recurrence interval trends reported in other studies following large earthquakes and with experimental work showing slip amplitudes and stress drop decrease with loading rate.

Temporal, spatial, and management variability in the carbon footprint of New Zealand milk.

The carbon footprint of milk from year-round grazed-pasture dairy systems and its variability has had limited research. The objective of this study was to determine temporal, regional, and farm system variability in the carbon footprint of milk from New Zealand (NZ) average dairy production. Farm production and input data were collected from a national database for 2010/11 to 2017/18 across regions of NZ and weighted on relative production supplied to the major dairy cooperative Fonterra to produce an NZ-average. Total greenhouse gas emissions were calculated using a life cycle assessment methodology for the cradle-to-farm gate, covering all on- and off-farm contributing sources. The NZ-average carbon footprint of milk varied from 0.81 kg of CO2 equivalent (CO2eq)/kg of fat- and protein-corrected milk (FPCM) in 2010/11 (with widespread drought) to 0.75 to 0.78 kg of CO2eq/kg of FPCM in 2013/14 to 2017/18, with a trend for a small decrease over time. Regional variation occurred with highest carbon footprint values for the Northland region due to greatest climatic and soil limitations on pasture production. Dairy cattle diet was approximately 85% from grazed pasture with up to 15% from brought-in feeds (mainly forages and by-products). The CO2 emissions from direct fuel and electricity use constituted <2% of total CO2eq emissions, whereas enteric methane was near 70% of the total. An estimate of potential contribution from direct land use change (plantation forest to pasture) was 0.13 kg of CO2eq/kg of FPCM. This was not included because nationally there has been a net increase in forest land and a decrease in pasture land over the last 20 yr. Data used were highly representative, as evident by the same estimated carbon footprint from 368 farms (in 2017/18) from the national database compared with that from a direct survey of 7,146 farms. New Zealand-specific nitrous oxide emission factors were used, based on many validated field trials and as used in the NZ greenhouse gas inventory, resulting in an 18% lower carbon footprint than if default Intergovernmental Panel on Climate Change factors had been used. Evaluation of the upper and lower quartiles of farms based on per-cow milk production (6,044 vs. 3,542 kg of FPCM/cow) showed a 15% lower carbon footprint for the upper quartile of farms, illustrating the potential for further decrease in carbon footprint with improved farm management practices.

A view of hydrogen/hydroxide flux across lipid membranes.

A topic emerging roughly 30 years ago and engendering an incompletely resolved controversy is reviewed in this article: the relatively high permeability and pH independence associated with H(+)/OH(-) passive movements across lipid membranes. We summarize the expected characteristics of simple H(+)/OH(-) diffusion and those of a reaction between H(+) and OH(-) being attracted from opposite surfaces and condensing in an interfacial zone of the membrane. An interfacial H(+)/OH(-) reaction mechanism gives the experimentally observed behavior of an H(+)/OH(-) flux that is independent of the pH measurement range. This mechanism assumes that H(+) and OH(-) within the interfacial zone become electrostatically aligned on opposite sides of the hydrophobic membrane core. Electrostatic attraction and charge delocalization among a small cluster of water molecules surrounding the ions reduce the Born energy for H(+)/OH(-) insertion into lipid. This transmembrane condensation model predicts the magnitude of the experimentally determined H(+)/OH(-) flux, which is significantly greater than that of other monovalent ions. The consequences of an elevated H(+)/OH(-) permeability compared to other ions and the relative pH independence of this flux have consequences for understanding the chemical evolution of life.

Earthquake slip on oceanic transform faults.

Oceanic transform faults are one of the main types of plate boundary, but the manner in which they slip remains poorly understood. Early studies suggested that relatively slow earthquake rupture might be common; moreover, it has been reported that very slow slip precedes some oceanic transform earthquakes, including the 1994 Romanche earthquake. The presence of such detectable precursors would have obvious implications for earthquake prediction. Here we model broadband seismograms of body waves to obtain well-resolved depths and rupture mechanisms for 14 earthquakes on the Romanche and Chain transform faults in the equatorial Atlantic Ocean. We found that earthquakes on the longer Romanche transform are systematically deeper than those on the neighbouring Chain transform. These depths indicate that the maximum depth of brittle failure is at a temperature of approximately 600 degrees C in oceanic lithosphere. We find that the body waves from the Romanche 1994 earthquake can be well modelled with relatively deep slip on a single fault, and we use the mechanism and depth of this earthquake to recalculate its source spectrum. The previously reported slow precursor can be explained as an artefact of uncertainties in the assumed model parameters.

Mitochondria shape hormonally induced cytoplasmic calcium oscillations and modulate exocytosis.

Pituitary gonadotropes transduce hormonal input into cytoplasmic calcium ([Ca(2+)](cyt)) oscillations that drive rhythmic exocytosis of gonadotropins. Using Calcium Green-1 and rhod-2 as optical measures of cytoplasmic and mitochondrial free Ca(2+), we show that mitochondria sequester Ca(2+) and tune the frequency of [Ca(2+)](cyt) oscillations in rat gonadotropes. Mitochondria accumulated Ca(2+) rapidly and in phase with elevations of [Ca(2+)](cyt) after GnRH stimulation or membrane depolarization. Inhibiting mitochondrial Ca(2+) uptake by the protonophore CCCP reduced the frequency of GnRH-induced [Ca(2+)](cyt) oscillations or, occasionally, stopped them. Much of the Ca(2+) that entered mitochondria is bound by intramitochondrial Ca(2+) buffering systems. The mitochondrial Ca(2+) binding ratio may be dynamic because [Ca(2+)](mit) appeared to reach a plateau as mitochondrial Ca(2+) accumulation continued. Entry of Ca(2+) into mitochondria was associated with a small drop in the mitochondrial membrane potential. Ca(2+) was extruded from mitochondria more slowly than it entered, and much of this efflux could be blocked by CGP-37157, a selective inhibitor of mitochondrial Na(+)-Ca(2+) exchange. Plasma membrane capacitance changes in response to depolarizing voltage trains were increased when CCCP was added, showing that mitochondria lower the local [Ca(2+)](cyt) near sites that trigger exocytosis. Thus, we demonstrate a central role for mitochondria in a significant physiological response.

Separate entry pathways for phosphate and oxalate in rat brain microsomes.

ATP-dependent (45)Ca uptake in rat brain microsomes was measured in intracellular-like media containing different concentrations of PO(4) and oxalate. In the absence of divalent anions, there was a transient (45)Ca accumulation, lasting only a few minutes. Addition of PO(4) did not change the initial accumulation but added a second stage that increased with PO(4) concentration. Accumulation during the second stage was inhibited by the following anion transport inhibitors: niflumic acid (50 microM), 4,4'-dinitrostilbene-2, 2'-disulfonic acid (DNDS; 250 microM), and DIDS (3-5 microM); accumulation during the initial stage was unaffected. Higher concentrations of DIDS (100 microM), however, inhibited the initial stage as well. Uptake was unaffected by 20 mM Na, an activator, or 1 mM arsenate, an inhibitor of Na-PO(4) cotransport. An oxalate-supported (45)Ca uptake was larger, less sensitive to DIDS, and enhanced by the catalytic subunit of protein kinase A (40 U/ml). Combinations of PO(4) and oxalate had activating and inhibitory effects that could be explained by PO(4) inhibition of an oxalate-dependent pathway, but not vice versa. These results support the existence of separate transport pathways for oxalate and PO(4) in brain endoplasmic reticulum.

Luminal Ca2+ protects against thapsigargin inhibition in neuronal endoplasmic reticulum.

Thapsigargin is a specific and potent inhibitor of sarco/endoplasmic reticulum Ca2+-ATPases. However, in whole rat brain microsomes, 1 microM thapsigargin had no significant effect on the 10-min time course of ATP-dependent Ca2+ uptake in the absence of the luminal Ca2+ chelator oxalate. In contrast, 50 mM oxalate resolved a thapsigargin-sensitive Ca2+ uptake rate (IC50 approximately 1 nM thapsigargin) five times that of a thapsigargin-insensitive rate. This remaining approximately 20% of the total ATP-dependent accumulation was insensitive to thapsigargin (up to 10 microM), slightly less sensitive to vanadate inhibition, and unresponsive to 5 microM inositol 1,4,5-trisphosphate or 10 mM caffeine. Measuring both 12-min Ca2+ uptake and initial Ca2+ uptake rates, the apparent thapsigargin sensitivity increased as oxalate concentrations increased from 10 to 50 mM, corresponding to a range of luminal free Ca2+ concentrations of approximately 300 down to 60 nM. Addition of oxalate during steady-state 45Ca accumulation rapidly resolved the aforementioned thapsigargin sensitivity. These results strongly suggest that luminal Ca2+ may protect a large portion of neuronal endoplasmic reticulum Ca2+ pumps against thapsigargin inhibition. Although high [Ca2+] has been previously shown to protect against thapsigargin inhibition in several reticular membrane preparations, our results suggest that luminal Ca2+ alone is responsible for mediating this effect in neurons.

Effects of the intraluminal Ca load on the kinetics of 45Ca uptake and efflux in brain microsomes.

Effects of increasing intraluminal Ca ([Ca]i) on the kinetics of rat brain microsomal uptake and efflux are reported here. Isolated rat brain microsomes accumulated 45Ca in an extravesicular free Ca ([Ca]o)- and ATP-dependent manner. Increased microsomal Ca load resulted in a decreased initial rate of 45Ca uptake and an increased tau, time to reach 63% of steady-state accumulation. Isolated rate brain microsomes lost 45Ca in a temperature- and [Ca]i-dependent manner. Whether preloaded with tracer 45Ca and either < or = 0.5 or 25 microM [Ca]o, the time constant of efflux was larger at 4 degrees C as compared with 37 degrees C. Additionally, increased microsomal Ca load resulted in a decreased time constant of 45Ca efflux. This shorter efflux time constant cannot explain the effect of [Ca]i on tau during uptake which was in fact longer for preloaded microsomes. Rather, these data suggest that, as Ca accumulates into unloaded microsomes, a steadily increasing [Ca]i slows unidirectional Ca influx (presumably by inhibiting the endoplasmic reticulum Ca pump) and enhances unidirectional Ca efflux, and that these combined effects ultimately shorten the time needed to achieve steady-state luminal [Ca]i.

Calcium chelators enhance 45Ca accumulation in permeablized synaptosomes and in microsomes.

The study of intracellular Ca2+ regulation usually requires using calcium chelators to adjust [Ca2+]. We examined the effects of these chelators on calcium accumulation in microsomes and saponin-permeabilized synaptosomes to assess their influence on apparent transport properties. At a fixed free Ca2+ of 0.6 microM, increasing ethylene glycol-bis(beta-aminoethyl ether)-N,N,N', N'-tetraacetic acid (EGTA) and total Ca2+ enhanced ATP-dependent 45Ca sequestration in synaptosomes and microsomes. The EGTA-Ca complex did not change the maximal initial calcium uptake rate or maximal steady-state accumulation. Rather, EGTA/Ca increased the apparent affinity of the microsomal transporter for Ca2+. The presence of the organic anion transport inhibitor probenicid (2.5 mM) had no effect on 45Ca accumulation in the presence of EGTA. Replacing part of the Ca2+ with Ni2+ but maintaining [Ca2+] approximately constant reduced 45Ca uptake, suggesting that the Ni-EGTA complex did not stimulate 45Ca transport. Our results imply that EGTA is not actively transported across the endoplasmic reticulum membrane, nor does the divalent ion-bound form of EGTA change the properties of the transporter. EGTA, and other mobile calcium chelators with similar structures, e.g., 1,2-bis(2-aminophenoxy)ethane-N,N,N',N'-tetraacetic acid, indo 1, and fluo 3, may increase calcium uptake by delivering more Ca2+ to its transport site.

Cytoplasmic calcium buffer capacity determined with Nitr-5 and DM-nitrophen.

We have examined intracellular calcium buffer capacity of cytoplasm from the giant axon of the marine invertebrate Myxicola infundibulum by photolytically releasing calcium from 'caged' compounds, while monitoring free calcium, [Ca2+], with Ca-sensing electrodes. In cytoplasm containing intact organelles, two features of the [Ca2+] response were seen upon light exposure: an initial spike from basal [Ca2+], followed by a slower phase recovery. Both the amplitude of the spike in [Ca2+] and the recovery were reduced by removal of MgATP. If organelles were removed from the cytoplasm, light exposure caused only a step-like change in [Ca2+] with no recovery. Apparent buffer capacities (delta bound Ca/delta free Ca) were unaffected by changing pH from 7.0 to 7.5; however, raising basal free calcium above 3 microM significantly reduced this parameter. The buffer capacity measured after the initial spike varied by as much as an order of magnitude from one giant axon to another but averaged approximately 50 in the absence and approximately 100 in the presence of 1 mM MgATP for [Ca2+] below 3 microM.

Calcium diffusion coefficient in Myxicola axoplasm.

Calcium diffusion coefficients were measured in Myxicola axoplasm and in agar controls by two independent techniques: one utilizing 45Ca, and one utilizing Ca-specific mini-electrodes. The lowest value, approximately 0.1 x 10(-6) cm2.s-1, was measured, using the mini-electrode technique, in axoplasm with intact Ca-sequestering organelles. With ATP-depleted axoplasm, diffusion coefficients of 0.5-2 x 10(-6) cm2.s-1 were obtained by both isotope and mini-electrode techniques. In organelle-free axoplasm with a protein concentration roughly half that in the intact axoplasm, diffusion coefficients of 1.4-3 x 10(-6) cm2.s-1 were measured at 0.7 microM Ca and 7 x 10(-6) cm2.s-1 at 3-5 microM Ca. When compared with measurements of the calcium buffering capacity [Al-Baldawi NF. Abercrombie RF. (1995) Cytoplasmic Ca buffer capacity determined with Nitr-5 and DM-nitrophen. Cell Calcium, 17, 409-422], these diffusion coefficients require that part of the buffer capacity be located on mobile Ca-binding sites.

Calcium accumulation by organelles within Myxicola axoplasm.

1. 45Ca2+ accumulation into inulin-inaccessible compartments within cytoplasm from the giant axon of Myxicola infundibulum was measured as a function of free calcium, pH, and time. Accumulation reached a maximum after 1 h and remained stable for at least 3 h. 2. At 0.5, 5, and 50 microM [Ca2+], in the presence of 1 mM ATP or 5 mM succinate, steady-state calcium uptake had a bell-shaped dependence on pH with a maximum near pH 7. Uptake was abolished by the proton uncoupling reagent carbonyl cyanide p-trifluoromethoxy-phenylhydrazone (FCCP, 4 micrograms ml-1). 3. Uptake of the membrane permeant cation, [14C]-tetraphenylphosphonium (TPP+), also had a bell-shaped dependence on pH with a maximum pH approximately 7, suggesting a pH dependence of the electrical potential of a membrane enclosed cytoplasmic compartment. Cyanide (2 mM) inhibited TPP+ uptake. 4. Inositol 1,4,5-trisphosphate (IP3, 10 microM), reduced steady-state calcium accumulation by 20-22% at 0.5 microM free calcium, pH 7 (P < 0.01, n = 16) and at 5 microM free calcium, pH 8 (P < 0.0005, n = 35). No effects of IP3 were found at other pH or calcium concentrations. 5. Neither guanosine 5'-triphosphate (GTP) nor inositol 1,3,4,5-tetrakisphosphate (IP4) had an effect on calcium uptake (5 microM [Ca2+], pH 8). 6. At 0.5 microM free calcium; vanadate (10 microM) inhibited 20-30%, of the 45Ca2+ accumulation, thapsigargin (33 nM) inhibited 20-30%, and cyanide (2 mM) plus oligomycin B (2 micrograms ml-1), or valinomycin (1 microM), inhibited 70-80%. The fraction of uptake sensitive to thapsigargin fell as the free calcium increased; however, the sensitivity of uptake to cyanide plus oligomycin B was approximately 80% for 0.5, 5.0, and 50 microM [Ca2+]. 7. Thapsigargin had no additional inhibiting effect in the presence of cyanide plus oligomycin B. IP3 had no effect in the presence of cyanide plus oligomycin B or other mitochondrial inhibitors. 8. Results suggest the presence of both mitochondrial (70-80%) and non-mitochondrial (20-30%) calcium pools in this system (at 0.5-5.0 microM Ca2+). The apparent non-mitochondrial uptake (sensitive to thapsigargin, or IP3) is not detectable in the presence of mitochondrial inhibitors. We interpret these results as evidence of functional communication between mitochondrial and non-mitochondrial calcium stores.

Cytoplasmic hydrogen ion diffusion coefficient.

The apparent cytoplasmic proton diffusion coefficient was measured using pH electrodes and samples of cytoplasm extracted from the giant neuron of a marine invertebrate. By suddenly changing the pH at one surface of the sample and recording the relaxation of pH within the sample, an apparent diffusion coefficient of 1.4 +/- 0.5 x 10(-6) cm2/s (N = 7) was measured in the acidic or neutral range of pH (6.0-7.2). This value is approximately 5x lower than the diffusion coefficient of the mobile pH buffers (approximately 8 x 10(-6) cm2/s) and approximately 68x lower than the diffusion coefficient of the hydronium ion (93 x 10(-6) cm2/s). A mobile pH buffer (approximately 15% of the buffering power) and an immobile buffer (approximately 85% of the buffering power) could quantitatively account for the results at acidic or neutral pH. At alkaline pH (8.2-8.6), the apparent proton diffusion coefficient increased to 4.1 +/- 0.8 x 10(-6) cm2/s (N = 7). This larger diffusion coefficient at alkaline pH could be explained quantitatively by the enhanced buffering power of the mobile amino acids. Under the conditions of these experiments, it is unlikely that hydroxide movement influences the apparent hydrogen ion diffusion coefficient.

Properties of calcium binding by Myxicola axoplasmic protein.

The 45Ca2+ binding properties of axoplasmic protein from the Myxicola giant axon have been investigated using a centrifugal/concentration-dialysis technique. Scatchard plot analysis of these binding data suggest that Ca2+ is attached to a site with an equilibrium dissociation constant of 7.7 +/- 0.5 microM and a capacity of 4.4 +/- 0.2 mumol/g axoplasmic protein (n = 11). Addition of other cations--Cd2+, Mn2+, Al3+, Cu2+, Ba2+, and Zn2(+)--at concentrations up to 10 microM did not displace 0.2 microM 45Ca2+ from its binding site, probably because of buffering of these cations by amino acid residues within the protein solutions. The protein could be stored at 4 degrees C for up to 16 days with no appreciable change in the number of calcium sites. Ca2+ binding equilibrium took place in less than 30 min of incubation. Increasing the incubation temperature from 4 degrees C to 37 degree C reduced the number of Ca2+ sites. The binding capacity was reduced by one-half when the protein was dialyzed with 4 M urea or high ionic strength KCl (2 M). Calcium binding was examined as a function of pH. When the protein was dialyzed overnight at different pH values and all the binding was done at pH 7.0, the apparent number of Ca2+ sites decreased as the pH of the dialysis medium was increased. When the protein was dialyzed overnight at pH 7.0 and the binding was done at different pH values, the apparent binding capacity increased as pH increased.(ABSTRACT TRUNCATED AT 250 WORDS)

Ca2+ binding by Myxicola neurofilament proteins.

Titrimetric, 45Ca dialysis, and autoradiographic methods were used to examine how axoplasmic proteins from the giant neuron of the marine annelid Myxicola infundibulum bind calcium. Following the autoradiographic method of Maruyama et al., the 150-160 kD neurofilament subunits were identified as prominent intracellular Ca-binding peptides. Using equilibrium dialysis, extracts of axoplasmic proteins (greater than 50% neurofilament subunits) were examined in 300 mM KCl at different concentrations of free Ca and Mg, and at different pH. Axoplasmic proteins showed a high affinity Ca binding site (K1/2 3-6 microM, capacity 3-7 mumole g-1 protein) at pH 6.8 or pH 7.5. Changing the Mg concentration from 0 to 5 mM had no effect on the Ca binding. Elevating the dialysis pH from 7.0 to 9.0 reduced the apparent number of binding sites for Ca. Using microelectrodes to record the free Ca, microtitrations of axoplasmic proteins were completed by adding small amounts of CaCl2 to 100 microliters volumes of protein solutions. In a medium containing ionic constituents closely resembling those of the Myxicola axon, a Ca binding capacity of 5.0 mumole g-1 protein and a K1/2 of approximately 1 microM were measured.

Free diffusion coefficient of ionic calcium in cytoplasm.

The free diffusion coefficient of ionic Ca was measured in isolated samples of Myxicola axoplasm by following the migration of 45Ca. When precautions were taken to minimize the sequestration and chelation of 45Ca (i.e., using inhibitors, energy deprivation, and saturation of Ca chelation sites), a diffusion coefficient of 5.3 x 10(-6) cm2 s-1 was measured. The diffusion coefficient was not appreciably changed by lowering free calcium from 100 microM to approximately 10 microM or by increasing the diffusion time from ten to twenty minutes. In untreated cytoplasm taken directly from the giant axon of Myxicola, the migration of Ca was more complex and could not be described by a single diffusion coefficient. This result is interpreted to suggest that bulk movement of Ca-buffers may occur in untreated Myxicola axoplasm, a system that contains few microtubules.

High cytosolic pH inhibits Ca uptake by Myxicola axon mitochondria.

Microliter samples of cytoplasm containing mitochondria were aspirated from giant axons of the marine annelid Myxicola infundibulum into polyethylene tubes. The small molecular constituents within these cytoplasmic samples were controlled by a dialysis capillary with a 6,000 molecular weight cut off. The negative log of the calcium ion activity (pCa) (6.72 +/- 0.03, n = 40) and, in some cases, the pH (7.51 +/- 0.01, n = 7) of the samples were monitored with ion-sensitive microelectrodes. Adding 5 mM succinate or 5 mM ATP at pH 7.5 caused the Ca activity in the cytoplasm to drop from an experimentally elevated value of approximately 10 microM to below 1 microM. This decrease could be inhibited with ruthenium red, suggesting a mitochondrial mechanism. Ca uptake, following the addition of either succinate or ATP, was reversibly slowed when the cytoplasmic pH was elevated to approximately 8.3. When ruthenium red was added after mitochondria had taken up Ca, the Ca activity in the extramitochondrial cytoplasm gradually increased suggesting ongoing release of Ca from storage sites. Increasing the cytoplasmic pH to approximately 8.5 in the presence of ruthenium red did not increase the ongoing release over that found with ruthenium red alone. The apparent washout of Ca from the energy-independent, nonmitochondrial Ca buffers was only slightly affected by pH (pH 7.5-8.5). It is concluded that elevating intracellular pH to 8.3 slows the Ca uptake by mitochondria. Thus cytoplasmic pH may have a function in regulating mitochondrial Ca metabolism and/or extramitochondrial calcium activity.

Calcium and proton buffering and diffusion in isolated cytoplasm from Myxicola axons.

Ion-selective electrodes recorded the pH (7.49 +/- 0.05, n = 8) and pCa (6.72 +/- 0.03, n = 40) in samples (approximately 1 microliter) of isolated Myxicola axoplasm mounted within 760-micron diameter plastic tubes. We determined the interactions between Ca2+ and H+ on axoplasmic buffers by microinjecting CaCl2 or HCl into the axoplasmic samples at a distance 75-125 micron from the tips of the electrodes (distance = r). When axoplasmic pH was lowered 0.97 +/- 0.095 from its resting value (measured at r = 125 micron) by injecting 4 nmol HCl, pCa dropped 0.30 +/- 0.05 (n = 6). When expressed in units of concentration, these data show that a HCl injection of approximately 4 mmol/l axoplasm increased H+ and Ca2+ activity by approximately 0.3 microM. Lowering axoplasmic pCa 2.20 +/- 0.43 (r = 75 micron) (n = 3) by injecting 40 pmol CaCl2 had only a small effect on pH. In other experiments, two Ca2+ electrodes measured the Ca2+ activity 125 and 375 micron from the site of CaCl2 injection. Evidence of Ca2+ buffering was obtained when the Ca2+ activity at these two locations was below that expected for simple Ca2+ diffusion away from the injection site. Centrifuged axoplasm (100,000 g) taken from the bottom of the centrifuge tube had a somewhat greater Ca2+ buffering capacity than that taken from the top of the tube. Electron microscopic studies of the centrifuged axoplasm showed a greater concentration of mitochondria and other axoplasmic vesicles in the bottom of the centrifuge tube. Ruthenium red (20-40 micrograms/ml) greatly reduced Ca2+ buffering. The mitochondrial inhibitors CN (2 mM) and oligomycin (a mixture of oligomycin A, B, and C, 5 micrograms/ml) also reduced Ca2+ buffering but were not as effective as ruthenium red. Axoplasm in which ATP and mitochondrial substrates were removed by dialysis was unable to lower free Ca2+ when the concentration of this ion was elevated to approximately 10 microM. In the presence of oligomycin to block mitochondrial ATPase, and with Mg2+ -ATP as the only source of energy, axoplasm lowered Ca2+ activity slowly; with succinate as the only metabolic substrate, axoplasm rapidly lowered the Ca2+ activity from approximately 10 microM to below 1 microM.