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碳质小行星中可能的核糖合成。

Possible Ribose Synthesis in Carbonaceous Planetesimals.

作者信息

Paschek Klaus, Kohler Kai, Pearce Ben K D, Lange Kevin, Henning Thomas K, Trapp Oliver, Pudritz Ralph E, Semenov Dmitry A

机构信息

Max Planck Institute for Astronomy, Königstuhl 17, 69117 Heidelberg, Germany.

Department of Chemistry, Ludwig-Maximilians-University Munich, Butenandtstr. 5-13, House F, 81377 Munich, Germany.

出版信息

Life (Basel). 2022 Mar 10;12(3):404. doi: 10.3390/life12030404.

Abstract

The origin of life might be sparked by the polymerization of the first RNA molecules in Darwinian ponds during wet-dry cycles. The key life-building block ribose was found in carbonaceous chondrites. Its exogenous delivery onto the Hadean Earth could be a crucial step toward the emergence of the RNA world. Here, we investigate the formation of ribose through a simplified version of the formose reaction inside carbonaceous chondrite parent bodies. Following up on our previous studies regarding nucleobases with the same coupled physico-chemical model, we calculate the abundance of ribose within planetesimals of different sizes and heating histories. We perform laboratory experiments using catalysts present in carbonaceous chondrites to infer the yield of ribose among all pentoses (5Cs) forming during the formose reaction. These laboratory yields are used to tune our theoretical model that can only predict the total abundance of 5Cs. We found that the calculated abundances of ribose were similar to the ones measured in carbonaceous chondrites. We discuss the possibilities of chemical decomposition and preservation of ribose and derived constraints on time and location in planetesimals. In conclusion, the aqueous formose reaction might produce most of the ribose in carbonaceous chondrites. Together with our previous studies on nucleobases, we found that life-building blocks of the RNA world could be synthesized inside parent bodies and later delivered onto the early Earth.

摘要

生命的起源可能是由达尔文池塘中首个RNA分子在干湿循环期间的聚合引发的。关键的生命构成要素核糖在碳质球粒陨石中被发现。它从外部输送到冥古宙的地球上可能是迈向RNA世界出现的关键一步。在此,我们通过碳质球粒陨石母体内部简化版的福莫司反应来研究核糖的形成。基于我们之前使用相同耦合物理化学模型对核碱基的研究,我们计算了不同大小和加热历史的小行星体内核糖的丰度。我们利用碳质球粒陨石中存在的催化剂进行实验室实验,以推断福莫司反应过程中形成的所有戊糖(5个碳原子)中核糖的产率。这些实验室产率用于调整我们的理论模型,该模型只能预测5个碳原子的总丰度。我们发现计算出的核糖丰度与在碳质球粒陨石中测量到的丰度相似。我们讨论了核糖化学分解和保存的可能性以及从小行星体中得出的时间和位置限制。总之,水相福莫司反应可能在碳质球粒陨石中产生了大部分核糖。连同我们之前对核碱基的研究,我们发现RNA世界的生命构成要素可以在母体内部合成,随后输送到早期地球上。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/eaf7/8955445/51cf467a4b66/life-12-00404-g001.jpg

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