Phosphorylation of Skeletal Muscle Pyruvate Dehydrogenase Phosphatase in Response to Insulin Stimulation

Pyruvate dehydrogenase phosphatase (PDP) regulates carbohydrate oxidation through the pyruvate dehydrogenase (PDH) complex. PDP activates PDH, enabling increased carbohydrate flux towards oxidative energy production. In culture myoblasts, both PDP1 and PDP2 undergo covalent activation in response to insulin–stimulation by protein kinase C delta (PKCδ). Our objective was to examine the effect of insulin on PDP phosphorylation and PDH activation in skeletal muscle. Intact rat extensor digitorum longus muscles were incubated (oxygenated at 25°C, 1g of tension) for 30min in basal or insulin–stimulated (10 mU/mL) media. PDH activity increased 58% following stimulation, (p=0.057, n=11). Serine phosphorylation of PDP1 (p=0.047) and PDP2 (p=0.006) increased by 29% and 48%, respectively (n=8), and mitochondrial PKCδ protein content was enriched by 45% in response to stimulation (p=0.0009, n=8). These data suggest that the insulin–stimulated increase in PDH activity in whole tissue is mediated through mitochondrial migration of PKCδ and subsequent PDP phosphorylation.

Algal and protozoan response to Holocene climate change and anthropogenic impact: a case study from Sluice Pond, MA

Sluice Pond is a small (18 ha) and deep (Zmax 20.0 m) partially meromictic, pond in Lynn, Massachusetts that contains a diverse dinocyst record since the early Holocene. High dinocyst concentrations, including morphotypes not previously described, as well as the preservation of several specimens of cellulosic thecae are attributed to low dissolved oxygen (DO) in the basin. The fossil protozoan record supports the interpretation- thecamoebians were unable to colonize the basin until the middle Holocene and only became abundant when the drought-induced lowstand oxygenated the bottom waters. Protozoans tolerant of low DO became abundant through the late Holocene as water levels rose and cultural eutrophication produced a sharp increase in biochemical oxygen demand (BOD) beginning in the 17th century. Recent sediments contain a dominance of Peridinium willei, indicating cultural eutrophication and the planktonic ciliate Codonella cratera and the thecamoebian Cucurbitella tricuspis in the deep basin. Above the chemocline however, a diverse difflugiid thecamoebian assemblage is present.