The leucine zipper may induce electrophoretic mobility anomalies without DNA bending

Numerous proteins bend DNA upon binding, a phenomenon of potential significance for regulation of gene expression and chromatin. DNA bending is commonly predicted from the presence of electrophoretic mobility anomalies in protein–DNA complexes. However, as compared with electrophoretic methods, several DNA binding oncoprotein families do not display comparable evidence of DNA bends in x-ray structural studies. Herein, circularization kinetics and affinity measurements with prebent DNA templates were employed to assess bending and DNA structural preferences for Max and other basic helix–loop–helix/leucine zipper proteins. In this way, proteins in the Myc/Max basic helix–loop–helix/leucine zipper family were found not to bend DNA in solution but to actually stabilize DNA in an unbent configuration that resists circularization. The mobility anomaly was found to be induced by the leucine zipper protein motif, rather than structural distortions of DNA. Thus rigid protein domain structures may induce anomalous electrophoretic mobility. Moreover, the energetic preference of non-DNA bending proteins for unbent templates suggests mechanisms whereby chromatin structure may regulate transcription.

Anomalies in coral reef community metabolism and their potential importance in the reef CO2 source-sink debate

It is not certain whether coral reefs are sources of or sinks for atmospheric CO2. Air–sea exchange of CO2 over reefs has been measured directly and inferred from changes in the seawater carbonate equilibrium. Such measurements have provided conflicting results. We provide community metabolic data that indicate that large changes in CO2 concentration can occur in coral reef waters via biogeochemical processes not directly associated with photosynthesis, respiration, calcification, and CaCO3 dissolution. These processes can significantly distort estimates of reef calcification and net productivity and obscure the contribution of coral reefs to global air–sea exchange of CO2. They may, nonetheless, explain apparent anomalies in the metabolic performance of reefs close to land and reconcile the differing experimental findings that have given rise to the CO2 debate.