Characterization of BseMII, a new type IV restriction–modification system, which recognizes the pentanucleotide sequence 5′-CTCAG(N)10/8↓

We report the properties of the new BseMII restriction and modification enzymes from Bacillus stearothermophilus Isl 15-111, which recognize the 5′-CTCAG sequence, and the nucleotide sequence of the genes encoding them. The restriction endonuclease R.BseMII makes a staggered cut at the tenth base pair downstream of the recognition sequence on the upper strand, producing a two base 3′-protruding end. Magnesium ions and S-adenosyl-l-methionine (AdoMet) are required for cleavage. S-adenosylhomocysteine and sinefungin can replace AdoMet in the cleavage reaction. The BseMII methyltransferase modifies unique adenine residues in both strands of the target sequence 5′-CTCAG-3′/5′-CTGAG-3′. Monomeric R.BseMII in addition to endonucleolytic activity also possesses methyltransferase activity that modifies the A base only within the 5′-CTCAG strand of the target duplex. The deduced amino acid sequence of the restriction endonuclease contains conserved motifs of DNA N6-adenine methylases involved in S-adenosyl-l-methionine binding and catalysis. According to its structure and enzymatic properties, R.BseMII may be regarded as a representative of the type IV restriction endonucleases.

Characteristics of the deep ocean carbon system during the past 150,000 years: ΣCO2 distributions, deep water flow patterns, and abrupt climate change

Studies of carbon isotopes and cadmium in bottom-dwelling foraminifera from ocean sediment cores have advanced our knowledge of ocean chemical distributions during the late Pleistocene. Last Glacial Maximum data are consistent with a persistent high-ΣCO2 state for eastern Pacific deep water. Both tracers indicate that the mid-depth North and tropical Atlantic Ocean almost always has lower ΣCO2 levels than those in the Pacific. Upper waters of the Last Glacial Maximum Atlantic are more ΣCO2-depleted and deep waters are ΣCO2-enriched compared with the waters of the present. In the northern Indian Ocean, δ13C and Cd data are consistent with upper water ΣCO2 depletion relative to the present. There is no evident proximate source of this ΣCO2-depleted water, so I suggest that ΣCO2-depleted North Atlantic intermediate/deep water turns northward around the southern tip of Africa and moves toward the equator as a western boundary current. At long periods (>15,000 years), Milankovitch cycle variability is evident in paleochemical time series. But rapid millennial-scale variability can be seen in cores from high accumulation rate series. Atlantic deep water chemical properties are seen to change in as little as a few hundred years or less. An extraordinary new 52.7-m-long core from the Bermuda Rise contains a faithful record of climate variability with century-scale resolution. Sediment composition can be linked in detail with the isotope stage 3 interstadials recorded in Greenland ice cores. This new record shows at least 12 major climate fluctuations within marine isotope stage 5 (about 70,000–130,000 years before the present).