Possible forcing of global temperature by the oceanic tides

An approximately decadal periodicity in surface air temperature is discernable in global observations from A.D. 1855 to 1900 and since A.D. 1945, but with a periodicity of only about 6 years during the intervening period. Changes in solar irradiance related to the sunspot cycle have been proposed to account for the former, but cannot account for the latter. To explain both by a single mechanism, we propose that extreme oceanic tides may produce changes in sea surface temperature at repeat periods, which alternate between approximately one-third and one-half of the lunar nodal cycle of 18.6 years. These alternations, recurring at nearly 90-year intervals, reflect varying slight degrees of misalignment and departures from the closest approach of the Earth with the Moon and Sun at times of extreme tide raising forces. Strong forcing, consistent with observed temperature periodicities, occurred at 9-year intervals close to perihelion (solar perigee) for several decades centered on A.D. 1881 and 1974, but at 6-year intervals for several decades centered on A.D. 1923. As a physical explanation for tidal forcing of temperature we propose that the dissipation of extreme tides increases vertical mixing of sea water, thereby causing episodic cooling near the sea surface. If this mechanism correctly explains near-decadal temperature periodicities, it may also apply to variability in temperature and climate on other times-scales, even millennial and longer.

Instability of repetitive DNA sequences: The role of replication in multiple mechanisms

Rearrangements between tandem sequence homologies of various lengths are a major source of genomic change and can be deleterious to the organism. These rearrangements can result in either deletion or duplication of genetic material flanked by direct sequence repeats. Molecular genetic analysis of repetitive sequence instability in Escherichia coli has provided several clues to the underlying mechanisms of these rearrangements. We present evidence for three mechanisms of RecA-independent sequence rearrangements: simple replication slippage, sister-chromosome exchange-associated slippage, and single-strand annealing. We discuss the constraints of these mechanisms and contrast their properties with RecA-dependent homologous recombination. Replication plays a critical role in the two slipped misalignment mechanisms, and difficulties in replication appear to trigger rearrangements via all these mechanisms.

Stabilization of diverged tandem repeats by mismatch repair: evidence for deletion formation via a misaligned replication intermediate.

A functional methyl-directed mismatch repair pathway in Escherichia coli prevents the formation of deletions between 101-bp tandem repeats with 4% sequence divergence. Deletions between perfectly homologous repeats are unaffected. Deletion in both cases occurs independently of the homologous recombination gene, recA. Because the methyl-directed mismatch repair pathway detects and excises one strand of a mispaired duplex, an intermediate for RecA-independent deletion of tandem repeats must therefore be a heteroduplex formed between strands of each repeat. We find that MutH endonuclease, which in vivo incises specifically the newly replicated strand of DNA, and the Dam methylase, the source of this strand-discrimination, are required absolutely for the exclusion of "homeologous" (imperfectly homologous) tandem deletion. This supports the idea that the heteroduplex intermediate for deletion occurs during or shortly after DNA replication in the context of hemi-methylation. Our findings confirm a "replication slippage" model for deletion formation whereby the displacement and misalignment of the nascent strand relative to the repeated sequence in the template strand accomplishes the deletion.