Implications of Microbial Thiosulfate Utilization in Red Clay Sediments of the Central Indian Basin: The Martian Analogy

Singh Tanya; Kshirsagar Pranav R.; Das Anindita; Yadav Kunal; Mallik Sweta; Mascarenhas‐Pereira M. B. L.; Thomas Tresa Remya A.; Shivaramu Mamatha S.; P. A. LokaBharathi; Khadge N. H.; Nath B. Nagender; Dhakephalkar Prashant K.; Iyer Sridhar D.; Ray Dwijesh; Valsangkar A. B.; Garg Anita; Prakash Babu C.; Waghole Ravindra J.; Waghmare Shailesh S.; Rajwade Jyutika M.; Paknikar Kishore M.

摘要

Abstract >Microbial thiosulfate utilization and S‐disproportionation could be important mechanisms of sulfate‐formations on Earth and Mars. Sulfates on Mars date back to late‐Noachian to Hesperian period. In contrast, the large sulfur/sulfate formations on Earth evolved under different chronological sequences. The S‐cycle was provoked intermittently, permitting multiple appearances of the S‐oxidizers on an evolutionary timescale. Hydrothermally altered deep‐oceanic red clay sediments of the Central Indian Basin were examined as potential analogue for sulfur (S) oxidation on Mars. The basin sediments supported an active microbial S‐metabolism that exhibited S‐disproportionation coupled to microbial carbon‐fixation through intermediate processes like thiosulfate utilization. Sulfur‐oxidizers/thiotrophic denitrifiers were isolated in large numbers at circum‐neutral pH, from these cold and dark abyssal Fe‐oxide dominated organic‐C starved clay. Experimental simulations under psychrophilic and thermo‐tolerant conditions revealed the coexistence of an anaerobic, thermal component under the predominantly oxic, circum‐neutral seafloor conditions. Multiple causative factors like hydrothermal seafloor circulation, in situ volcanism, and fracture zone reactivation could drive the widespread S‐cycle activity in the Central Indian Basin, albeit at a low scale. It is postulated that these conditions are analogous to Great Oxidation Event situations on Earth, when S‐oxidizers evolved and flourished. Experimental studies on microbial thiosulfate flux are few in spite of intense scientific interest in microbial S‐disproportionation. To the best of our knowledge, this is a new report on regression model development for microbial thiosulfate flux. These clay‐systems and their component microbes could serve as analogue to the ancient well‐hydrated Noachian Mars and throw light on planetary hydration and desiccation mechanisms. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >微生物硫代硫酸盐利用和S-歧化可能是地球和火星上硫酸盐形成的重要机制。火星上的硫酸盐返回到霍累累的晚期。相比之下，地球上的大型硫/硫酸盐形成在不同的时间顺序下演化。 S循环间歇地引发，允许S-氧化剂的多个出场在进化时间尺度上。中央印度盆地的热水改变的深海洋红粘土沉积物被检查为MARS上硫氧化的潜在类似物。盆地沉积物支持活性微生物S-代谢，其通过硫代硫酸盐利用等中间方法表现出与微生物碳固定相结合的S歧化。硫 - 氧化剂/肾冰茶的脱氮剂在循环中性pH下分离出大量的，来自这些冷和暗深度氧化物固定的有机-C饥饿的粘土。在心理学和热耐受条件下的实验模拟显示了厌氧，热部件在主要氧，周的中性海底条件下的共存。诸如水热海底循环，原位火山和骨折区重新激活等多种致病因素可以推动中央印度盆地的广泛S循环活动，尽管低规模。假设这些条件类似于地球上的大氧化事件情况，当S氧化剂演变和繁荣时。尽管对微生物S歧化的强烈科学感兴趣，但微生物硫代硫酸盐通量的实验研究很少。据我们所知，这是对微生物硫代硫酸盐通量的回归模型开发的新报告。这些粘土系统及其组分微生物可以作为模拟到古代水煮的Noachian火星，并在行星水合和干燥机制上抛光。</ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共22页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Singh Tanya&option=202" target="_blank" rel="nofollow">Singh Tanya;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kshirsagar Pranav R.&option=202" target="_blank" rel="nofollow">Kshirsagar Pranav R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Das Anindita&option=202" target="_blank" rel="nofollow">Das Anindita;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yadav Kunal&option=202" target="_blank" rel="nofollow">Yadav Kunal;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mallik Sweta&option=202" target="_blank" rel="nofollow">Mallik Sweta;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mascarenhas‐Pereira M. B. L.&option=202" target="_blank" rel="nofollow">Mascarenhas‐Pereira M. B. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thomas Tresa Remya A.&option=202" target="_blank" rel="nofollow">Thomas Tresa Remya A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shivaramu Mamatha S.&option=202" target="_blank" rel="nofollow">Shivaramu Mamatha S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P. A. LokaBharathi&option=202" target="_blank" rel="nofollow">P. A. LokaBharathi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Khadge N. H.&option=202" target="_blank" rel="nofollow">Khadge N. H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nath B. Nagender&option=202" target="_blank" rel="nofollow">Nath B. Nagender;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dhakephalkar Prashant K.&option=202" target="_blank" rel="nofollow">Dhakephalkar Prashant K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iyer Sridhar D.&option=202" target="_blank" rel="nofollow">Iyer Sridhar D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ray Dwijesh&option=202" target="_blank" rel="nofollow">Ray Dwijesh;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valsangkar A. B.&option=202" target="_blank" rel="nofollow">Valsangkar A. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Garg Anita&option=202" target="_blank" rel="nofollow">Garg Anita;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Prakash Babu C.&option=202" target="_blank" rel="nofollow">Prakash Babu C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Waghole Ravindra J.&option=202" target="_blank" rel="nofollow">Waghole Ravindra J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Waghmare Shailesh S.&option=202" target="_blank" rel="nofollow">Waghmare Shailesh S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rajwade Jyutika M.&option=202" target="_blank" rel="nofollow">Rajwade Jyutika M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Paknikar Kishore M.&option=202" target="_blank" rel="nofollow">Paknikar Kishore M.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Physical Research LaboratoryAhmedabad India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Council of Scientific and Industrial Research‐National Institute of OceanographyDona Paula India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> <p>Agharkar Research Institute‐Maharashtra Association for the Cultivation of SciencePune India;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thiosulfate&option=203" rel="nofollow">thiosulfate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=microbe&option=203" rel="nofollow">microbe;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mars&option=203" rel="nofollow">Mars;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=analogue&option=203" rel="nofollow">analogue;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sulfur‐disproportionation&option=203" rel="nofollow">sulfur‐disproportionation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Central Indian Basin&option=203" rel="nofollow">Central Indian Basin;</a> </p> <div class="translation"> 机译：硫代硫酸盐;微生物;火星;模拟;硫磺 - 歧视;中央印度盆地; 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H. ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li, H. &option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li, H. ,</a> <span>1987</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：中太平洋深海盆地红粘土微观结构：对亚壳核废物处置的意义</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201296670103.html">成都盆地红土沉积物中黏土矿物的特征及其古气候指示意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵璐璐&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵璐璐</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=洪汉烈&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,洪汉烈</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=殷科&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,殷科</a> <span> <a href="/journal-cn-56880/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质科技情报 </a> </span> <span> . 2015</span><span>,第3期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_gold_thesis/0201293406173.html">在碱性无氨硫代硫酸盐溶液中铜（Ⅱ）、碳酸盐和亚硫酸盐对金的浸出和硫代硫酸盐氧化分解的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐祥彬（翻译）&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 徐祥彬（翻译）</a> <span> <a href="/journal-cn-7991/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 黄金 </a> </span> <span> . 2009</span><span>,第4期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_marine-geology_thesis/0201272688209.html">利用叠前地震数据估算印度KG盆地含水合物沉积物的孔隙度</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rima Chatterjee1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 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href="/conference-cn-40845/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第三届生态毒理学学术研讨会 </a> <span> <span> . 2016</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020312386052.html">西南太平洋劳盆地(Lau Basin)深海热液区沉积物中微生物多样性及多环芳烃降解微生物的初步研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=董纯明&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 董纯明</a> <span> . 2009</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120106457626.html">用于捕捉通过生物介质的声和电磁场的作用在初始晶体结构中诱导的变化的方法和用于执行所述方法的装置、用于在复制晶体的结构中复制初始晶体结构的变化的方法(变型)和用于执行所述方法的装置(变型)、用于对生物对象施加影响的方法(变型)和用于执行所述方法的装置</a> <b>[P]</b> . <span> 中国专利： CN102256664A </span> <span> . 2011-11-23</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120113664604.html">一种pH和DO变化对水库沉积物中氮磷营养盐释放强度影响的方法</a> <b>[P]</b> . <span> 中国专利： CN113702312A </span> <span> . 2021-11-26</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130458353745.html">Use of heavily dewatered, possibly contaminated sediments and / or fine sediments separated from them, optionally contaminated, in the form of components for the subaquatic filling of water to be drained, in particular harbor basins</a> <b>[P]</b> . <span> 外国专利：  DE4331364A1 </span> <span> . 1995-03-16</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：使用严重脱水，可能被污染的沉积物和/或与其分离的细小沉积物（可选地被污染），其形式为用于水下排放的水下水填充物，特别是港口盆地 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130400131962.html">METHOD FOR DETECTING CLAYS IN A SEDIMENT BASIN BY SPECTROMETRIC MEASUREMENTS</a> 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