论文标题
在金星大气中检测最简单的氨基酸甘氨酸
Detection of simplest amino acid glycine in the atmosphere of Venus
论文作者
论文摘要
氨基酸被认为是化学中的主要成分,导致生命。甘氨酸是最简单的氨基酸,最常见于动物蛋白质中。这是一种糖原和非必需的氨基酸,是由活体自然产生的,在创造其他几种重要的生物化合物和蛋白质中起着关键作用。我们报告了最简单的氨基酸甘氨酸(NH $ _ {2} $ CH $ _ {2} $ COOH)的旋转吸收系的首次光谱检测,并使用Atacama大型米计/亚米计(Alma)的档案数据中的VENUS中的Venus中的I和II中的II和II。我们检测到NH $ _ {2} $ CH $ _ {2} $ cOOH的11个旋转吸收线之间的频率范围$ν$ = 245 $ -245 $ - $ 262 GHz,$ \ geq $ 3 $σ$统计意义。我们计算金星大气中的甘氨酸的总柱密度为$ n $(nh $ _ {2} $ ch $ _ {2} $ _ {2} $ cOOH)$ \ sim $ \ sim $ 5 $ \ times $ 10 $^{14} $ cm $ $ $^{ - 2} $。使用甘氨酸的色谱柱密度信息,我们计算了甘氨酸的丰度为$ \ sim $ 1.6 $ \ times $ 10 $^{ - 9} $在金星的气氛中。在金星大气中检测甘氨酸可能是了解金星大气中益生元分子的形成机理的关键之一。甘氨酸的检测表明,金星的上层大气可能与数十亿年前的生物学方法相同。
Amino acids are considered to be prime ingredients in chemistry, leading to life. Glycine is the simplest amino acid and most commonly found in animal proteins. It is a glucogenic and non-essential amino acid that is produced naturally by living bodies and plays a key role in the creation of several other important bio-compounds and proteins. We report the first spectroscopic detection of the rotational absorption lines of the simplest amino acid glycine (NH$_{2}$CH$_{2}$COOH) with confirmer I and II in the atmosphere of Venus using the archival data from the Atacama Large Millimeter/Submillimeter Array (ALMA). We detect the eleven rotational absorption lines of NH$_{2}$CH$_{2}$COOH between the frequency range of $ν$ = 245$-$262 GHz with $\geq$3$σ$ statistical significance. We calculate the total column density of glycine in the atmosphere of Venus is $N$(NH$_{2}$CH$_{2}$COOH) $\sim$ 5$\times$10$^{14}$ cm$^{-2}$. Using the column density information of glycine, we calculate the abundance of glycine is $\sim$ 1.6$\times$10$^{-9}$ in the atmosphere of Venus. The detection of glycine in the atmosphere of Venus might be one of the keys to an understanding of the formation mechanisms of prebiotic molecules in the atmosphere of Venus. The detection of glycine indicates that the upper atmosphere of Venus may be going through nearly the same biological method as Earth billions of years ago.