Millan Maëva, Campbell Kathleen A, Sriaporn Chanenath, Handley Kim M, Teece Bronwyn L, Mahaffy Paul, Johnson Sarah S
Department of Biology, Georgetown University, Washington, District of Columbia, USA.
Laboratoire Atmosphère, Observations Spatiales (LATMOS), LATMOS/IPSL, UVSQ Université Paris-Saclay, Sorbonne Université, CNRS, Guyancourt, France.
Astrobiology. 2025 Mar;25(3):225-252. doi: 10.1089/ast.2024.0020. Epub 2025 Feb 27.
Digitate siliceous sinter deposits are common in geothermal environments. They form via evaporation and precipitation of cooling silica-rich fluids and passive microbial templating. Increasing interest in these "finger-like" microstromatolitic sinters is related to their morphological and mineralogical resemblance to opaline silica-rich rocks discovered by NASA's Spirit rover in the Columbia Hills, Gusev crater, Mars. However, these terrestrial deposits remain understudied, specifically in terms of biosignature content and long-term preservation potential. In this study, six digitate, opaline (opal-A) sinter deposits were collected from five Taupō Volcanic Zonegeothermal fields, and their lipid biosignatures were investigated as Mars analogs. Samples were collected in pools and discharge channels of varied temperatures, pH, and water chemistries, with spicular to nodular morphologies. Results revealed the presence of biomarkers from unsilicified and silicified communities populating the hot spring sinters, including lipids from terrigenous plants, algae, and bacteria. Although DNA sequencing suggests that the composition and diversity of microbial communities are correlated with temperature, pH, and water chemistry of the springs, these environmental parameters did not seem to affect lipid recovery. However, the morphology of the sinters did play a role in lipid yield, which was higher in the finest, needle-like spicules in comparison to the broad, knobby sinters. The capability of current Mars flight mission techniques such as pyrolysis-gas chromatography-mass spectrometry to detect lipid biomarkers was also evaluated from a subset of samples in a pilot study under flight conditions. The early preservation of lipids in the studied sinters and their detection using flight-like techniques suggest that martian siliceous deposits are strong candidates for the search for biosignatures on Mars.
树枝状硅质泉华沉积物在地热环境中很常见。它们通过富含二氧化硅的冷却流体的蒸发和沉淀以及被动微生物模板作用形成。人们对这些“手指状”微叠层石泉华的兴趣日益增加,这与它们在形态和矿物学上与美国国家航空航天局的“勇气号”火星车在火星古谢夫环形山的哥伦比亚山发现的富含蛋白石二氧化硅的岩石相似有关。然而,这些陆地沉积物仍未得到充分研究,特别是在生物标志物含量和长期保存潜力方面。在这项研究中,从陶波火山带的五个地热场收集了六个树枝状、蛋白石(蛋白石-A)泉华沉积物,并将它们的脂质生物标志物作为火星类似物进行了研究。样本采集于温度、pH值和水化学性质各异的水池和排放通道中,形态从针状到结节状不等。结果显示,在温泉泉华中存在来自未硅化和硅化群落的生物标志物,包括来自陆生植物、藻类和细菌的脂质。虽然DNA测序表明微生物群落的组成和多样性与泉水的温度、pH值和水化学性质相关,但这些环境参数似乎并未影响脂质的回收率。然而,泉华的形态确实对脂质产量有影响,与宽阔的瘤状泉华相比,最细的针状泉华中脂质产量更高。在一项初步研究中,还在飞行条件下从一部分样本中评估了当前火星飞行任务技术(如热解气相色谱-质谱法)检测脂质生物标志物的能力。所研究的泉华中脂质的早期保存情况以及使用类似飞行技术对其进行的检测表明,火星硅质沉积物是在火星上寻找生物标志物的有力候选对象。