缓慢的冻融循环增强了千碱基 DNA 与长互补粘性末端的杂交

IF 3.1 Q2 CHEMISTRY, MULTIDISCIPLINARY
Dr. Natsumi Noda, Kohei Nomura, Naho Takahashi, Dr. Fumitaka Hashiya, Prof. Dr. Hiroshi Abe, Prof. Dr. Tomoaki Matsuura
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引用次数: 0

摘要

大型信息分子的产生可能在生命起源过程中起到了至关重要的作用。在这项研究中,我们进行了缓慢的冻融(F/T)实验,以测试在亚纳摩尔浓度下千倍碱基大小的DNA片段所连接的互补粘性末端之间杂交增强的可能性。2 千碱基对(kbp)和 3 千碱基对(kbp)的 DNA 片段与可形成 5 kbp 大小杂交产物的 50 碱基互补粘性末端混合。虽然简单的孵育几乎不会产生杂交产物,但在以可控的时间速率(<0.3 K min-¹)进行冷冻和解冻后,即使 DNA 的浓度很小(<1 nM),也能观察到明显有效的杂交。此外,缓慢解冻比缓慢冷冻对杂交的影响更大。快速解冻比缓慢解冻降低了反应效率,这表明共晶相浓度在杂交中起着重要作用。即使是两个 10 kbp DNA 片段之间的杂交反应,慢速 F/T 循环也很有效,在亚纳摩尔浓度下可产生 20 kbp 的产物。重复慢速 F/T 循环大大提高了反应效率。本文讨论了 F/T 循环在早期地球环境中可能发挥的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Slow Freeze-Thaw Cycles Enhanced Hybridization of Kilobase DNA with Long Complementary Sticky Ends

Slow Freeze-Thaw Cycles Enhanced Hybridization of Kilobase DNA with Long Complementary Sticky Ends

The creation of large information molecules may have played an essential role in the origins of life. In this study, we conducted slow freeze-thaw (F/T) experiments to test the possibility of enhanced hybridization between the complementary sticky ends attached to kilobase-sized DNA fragments at sub-nanomolar concentrations. DNA fragments of 2- and 3-kilobase pairs (kbp) with 50-base complementary sticky ends that can form 5 kbp-sized hybridization products were mixed. While simple incubation provided little hybridization product, significantly effective hybridization was observed after freezing and thawing at a controlled time rate (<0.3 K min−1), even with small DNA concentrations (<1 nM). Furthermore, slow thawing had a more effect on hybridization than slow freezing. The reaction efficiency was reduced by rapid thawing instead of slow thawing, suggesting that the eutectic phase concentration played an important role in hybridization. A slow F/T cycle was effective even for the hybridization reaction between two 10 kbp DNA fragments, which yielded a 20 kbp product at sub-nanomolar concentrations. Repeating the slow F/T cycle significantly improved the reaction efficiency. The possible role of the F/T cycles in early Earth environments is discussed here.

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