The effect of swimming activity on bone architecture in growing rats

The effect of non-habitual physical activity on bone architecture in the rat humeral shaft was examined. Two groups of rats were trained to swim for 1 h a day, for 20 weeks, at two training levels. The control group consisted of sedentary rats. Parameters of cross-sectional bone morphology (cross-section areas, principal area moments of inertia and their ratio) were used to evaluate the response of bone architecture to mechanical loading. The strength of bone was assessed by measuring the ultimate compressive force and stress. The cortical cross-section area and principal moments of inertia were found to be significantly higher in the swimming groups than in the controls. Examination of the ratio between the major and minor moments of inertia revealed a pronounced change in the shape of the bone cross-section which became more rounded following swimming training. The ultimate compressive force was significantly higher in the swimming rats while the changes in ultimate stress were not significant. Our results indicate a gain of bone strength due to increased periosteal apposition and modified bone tissue distribution. The marked changes in bone morphology are attributed to the different nature of the forces and moments exerted on the humerus during swimming compared to those prevailing during normal locomotion.     

Exogenous, but not endogenous, cyclic GMP reduces hepatic pyruvate kinase activity

We investigated the effects of exogenous cyclic GMP and stimulants of endogenous cyclic GMP accumulation on L-form (hepatic) pyruvate kinase (ATP: pyruvate 2-O-phosphotransferase, EC 2.7.1.40) activity in isolated rat hepatocytes. Exogenous cyclic GMP (200 muM) reduced pyruvate kinase activity, but was less potent than exogenous cyclic AMP (50 muM) (Ki congruent to 120 muM vs. 30 muM, respectively), had a slower onset of action (1.0 vs. 0.3 min, respectively) and a less rapid maximal effect (5.0 vs. 1.0 min, respectively). Similar results were noted with dibutyryl cyclic GMP or dibutyryl cyclic AMP. 1.0 muM acetylcholine increased cyclic GMP concentrations in isolated hepatocytes from 233 +/- 16 to 447 +/- 3 pmol/g cell protein (P less than 0.001), but did not alter pyruvate kinase activity. Similar results were noted with carbamylcholine, NaN3 or acetylcholine plus eserine sulfate. The results suggest a differential effect of exogenous vs. endogenous cyclic GMP on L-form pyruvate kinase activity, and question the physiological relevance of observations with exogenous cyclic GMP in this system.     

The effects of nonsuppressible insulin-like protein (NSILP) on cyclic nucleotide metabolism in rat liver.

Nonsuppressible insulin-like protein (NSILP), 100 ng/ml, inhibited cyclic AMP accumulation in rat liver, as stimulated by glucagon, 10^?7M, from 493 ± 12 to 183 ± 7 pmoles/gm tissue (p<0.001), but did not alter basal levels of cyclic AMP, 143 ± 2 pmoles/gm tissue. NSILP, 100 ng/ml, also inhibited cyclic AMP accumulation, stimulated by epinephrine, 5 × 10^?4M, from 387 ± 12 to 233 ± 9 pmoles/gm tissue. With 1 μM as substrate, NSILP, 100 ng/ml, increased cAMP-dependent phosphodiesterase activity in liver slices from 19.08 ± 0.18 to 24.94 ± 0.38 pmoles cAMP hydrolyzed/mg protein/min (p<0.001), but did not alter this enzyme activity in broken cell preparations of rat liver. Cyclic GMP levels in liver slices, 22.5 ± 0.3 pmoles/gm tissue, were increased by NSILP to 36.3 ± 0.5 pmoles/gm tissue (p<0.01). NSILP had no effect on adenylate cyclase activity. These changes, caused by NSILP in cyclic nucleotide metabolism in liver, resemble those described for insulin, and suggest that alterations in cyclic nucleotide levels in liver may be relevant to other hepatic effects of NSILP.     

Does carnitine have a role in fat absorption?

The effect of D-carnitine and tetradecylglycidic acid (TDGA), an inhibitor of carnitine palmitoyltransferase, on intestinal absorption of palmitic acid was determined. The proximal intestinal segment was ligated in adult male rats and filled with 0.5 microCi of 14C-palmitic acid alone or with either D-carnitine or TDGA. Thirty minutes later the radioactivity was determined in the intestinal lumen, intestinal wall and plasma. The absorption of palmitic acid was decreased in the presence of D-carnitine (10 mg/ml) as evidenced by significantly lower levels of radioactivity in the gut wall and the plasma and by significantly greater residual radioactivity in the lumenal contents. L-carnitine had no effect on plasma radioactivity but if D- and L-carnitine were given together the effect of D-carnitine was still in evidence. TDGA also inhibited intestinal absorption of palmitic acid.     

Terrigenous sediment-dominated reef platform infilling: an unexpected precursor to reef island formation and a test of the reef platform size–island age model in the Pacific

Low-lying coral reef islands are considered highly vulnerable to climate change, necessitating an improved understanding of when and why they form, and how the timing of formation varies within and among regions. Several testable models have been proposed that explain inter-regional variability as a function of sea-level history and, more recently, a reef platform size model has been proposed from the Maldives (central Indian Ocean) to explain intra-regional (intra-atoll) variability. Here we present chronostratigraphic data from Pipon Island, northern Great Barrier Reef (GBR), enabling us to test the applicability of existing regional island evolution models, and the platform size control hypothesis in a Pacific context. We show that reef platform infilling occurred rapidly (~4–5 mm yr⁻¹) under a “bucket-fill” type scenario. Unusually, this infilling was dominated by terrigenous sedimentation, with platform filling and subsequent reef flat formation complete by ~5000 calibrated years BP (cal BP). Reef flat exposure as sea levels slowly fell post highstand facilitated a shift towards intertidal and subaerial-dominated sedimentation. Our data suggest, however, a lag of ~1500 yr before island initiation (at ~3200 cal BP), i.e. later than that reported from smaller and more evolutionarily mature reef platforms in the region. Our data thus support: (1) the hypothesis that platform size acts to influence the timing of platform filling and subsequent island development at intra-regional scales; and (2) the hypothesis that the low wooded islands of the northern GBR conform to a model of island formation above an elevated reef flat under falling sea levels.

     

Contribution of sea ice microbial production to Antarctic benthic communities is driven by sea ice dynamics and composition of functional guilds

Organic matter produced by the sea ice microbial community (SIMCo) is an important link between sea ice dynamics and secondary production in near‐shore food webs of Antarctica. Sea ice conditions in McMurdo Sound were quantified from time series of MODIS satellite images for Sept. 1 through Feb. 28 of 2007–2015. A predictable sea ice persistence gradient along the length of the Sound and evidence for a distinct change in sea ice dynamics in 2011 were observed. We used stable isotope analysis (δ¹³C and δ¹⁵N) of SIMCo, suspended particulate organic matter (SPOM) and shallow water (10–20 m) macroinvertebrates to reveal patterns in trophic structure of, and incorporation of organic matter from SIMCo into, benthic communities at eight sites distributed along the sea ice persistence gradient. Mass‐balance analysis revealed distinct trophic architecture among communities and large fluxes of SIMCo into the near‐shore food web, with the estimates ranging from 2 to 84% of organic matter derived from SIMCo for individual species. Analysis of patterns in density, and biomass of macroinvertebrate communities among sites allowed us to model net incorporation of organic matter from SIMCo, in terms of biomass per unit area (g/m²), into benthic communities. Here, organic matter derived from SIMCo supported 39 to 71 per cent of total biomass. Furthermore, for six species, we observed declines in contribution of SIMCo between years with persistent sea ice (2008–2009) and years with extensive sea ice breakout (2012–2015). Our data demonstrate the vital role of SIMCo in ecosystem function in Antarctica and strong linkages between sea ice dynamics and near‐shore secondary productivity. These results have important implications for our understanding of how benthic communities will respond to changes in sea ice dynamics associated with climate change and highlight the important role of shallow water macroinvertebrate communities as sentinels of change for the Antarctic marine ecosystem.