RESUMO
DNA Computing is a rapidly-developing interdisciplinary area which could benefit from more experimental results to solve practical problems with the current biological tools. In this study, we have integrated microelectronics and molecular biology techniques for the storage of information and basic arithmetic operations via DNA. Using 16 different complementary sequences of DNA, we stored 4 bits of information on an electronic microarray and read the data via the fluorescent signal strength coming from the microarray pads. We also showed the possibility of addition and subtraction of quantities of fluorescently tagged DNA determined via their fluorescent signal strength. We conclude that the hybrid technology we employed, based on a matured Si-CMOS platform, has the potential to strengthen the pursuit of DNA Computation as well as finding its own niche applications.
Assuntos
Computadores Moleculares , DNA/química , Análise em Microsséries , Hibridização de Ácido Nucleico/métodos , DNA/genética , DNA/metabolismo , Eletrodos , Corantes Fluorescentes/químicaRESUMO
DNA Computing is a rapidly-developing interdisciplinary area which could benefit from more experimental results to solve practical problems with the current biological tools. In this study, we have integrated microelectronics and molecular biology techniques for the storage of information and basic arithmetic operations via DNA. Using 16 different complementary sequences of DNA, we stored 4 bits of information on an electronic microarray and read the data via the fluorescent signal strength coming from the microarray pads. We also showed the possibility of addition and subtraction of quantities of fluorescently tagged DNA determined via their fluorescent signal strength. We conclude that the hybrid technology we employed, based on a matured Si-CMOS platform, has the potential to strengthen the pursuit of DNA computation as well as finding its own niche applications.
Assuntos
Computadores Moleculares , DNA/química , Análise de Sequência com Séries de Oligonucleotídeos/instrumentação , Processamento de Sinais Assistido por Computador/instrumentação , Desenho de Equipamento , Análise de Falha de Equipamento , Integração de SistemasRESUMO
Major hydrocarbon accumulations occur in traps associated with salt domes. Whereas some of these hydrocarbons remain to be extracted for economic use, significant amounts have degraded in the subsurface, yielding mineral precipitates as byproducts. Salt domes of the Gulf of Mexico Basin typically exhibit extensive deposits of carbonate that form as cap rock atop salt structures. Despite previous efforts to model cap rock formation, the details of subsurface reactions (including the role of microorganisms) remain largely unknown. Here we show that cap rock mineral precipitation occurred via closed-system sulfate reduction, as indicated by new sulfur isotope data. 13C-depleted carbonate carbon isotope compositions and low clumped isotope-derived carbonate formation temperatures indicate that microbial, sulfate-dependent, anaerobic oxidation of methane (AOM) contributed to carbonate formation. These findings suggest that AOM serves as an unrecognized methane sink that reduces methane emissions in salt dome settings perhaps associated with an extensive, deep subsurface biosphere.