2025 Jessberger Award to Prof. Vinciane Debaille

IF 2.4 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Allan Treiman, Susanne P. Schwenzer, Alan Brandon, James M. D. Day, Richard J. Walker
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We are delighted today that our colleagues share our judgment and that Vinciane will receive the 2025 Jessberger Award.</p><p>She then discovered that other planetary bodies have basalts, too, and need isotope geochemists! This is when she came to Houston in 2005 as a postdoc, working with Dr. Alan Brandon at NASA JSC to learn about (among others) extinct radioisotope chronometry and geochemistry. That collaboration led to three foundational papers that demonstrated Dr. Debaille's analytical prowess, her ability to make sense of complementary short- and long-lived isotope systems, and her skill at presenting elegant and understandable interpretations. Those three laid the foundation for her hugely successful career in meteorite and planetary sciences.</p><p>The first paper from her post-doctoral work, published in <i>Nature</i> (Debaille et al., <span>2007</span>) in 2007, used high-precision analyses of the <sup>142</sup>Nd/<sup>144</sup>Nd and <sup>143</sup>Nd/<sup>144</sup>Nd ratios of shergottite martian meteorite to show that Mars likely experienced differentiation through progressive crystallization of a magma ocean within about 100 million years of core formation.</p><p>The second paper, in 2008 in <i>Earth and Planetary Science Letters</i> (Debaille et al., <span>2008</span>), added <sup>176</sup>Hf/<sup>177</sup>Hf data to the shergottite Nd story. There, she showed that the shergottites developed from mixtures of material enriched and depleted in incompatible trace elements, and implicated garnet fractionation in their sources.</p><p>The third of these seminal papers, 2009 in <i>Nature Geoscience</i> (Debaille et al., <span>2009</span>), attacked the other martian meteorites, the nakhlites. From their isotopic systematics, short- and long-lived, Dr. Debaille inferred an early overturn of the martian mantle. These three papers have become the background, the environment, for all subsequent studies of Mars' early evolution.</p><p>After her enormously successful time in Houston, Dr. Debaille returned to Belgium to the Université Libre de Bruxelles, first as a postdoc and then to her current position as Senior Research Associate (Maître de recherche). In Brussels, she has continued her work on the isotopic characteristics of both meteorites and terrestrial systems, many in collaboration with students—at least 14 doctoral and 18 masters. Her works are far too numerous to read out here; they extend from familiar planetary and meteorite subjects to less-expected topics like non-traditional isotopes (like Fe and Zn), Fe–Ti ore deposits, banded iron formations, archaean granitoids, and blue ice.</p><p>Among Dr. Debaille's papers, one in particular (special to me) connects the terrestrial and planetary realms (Debaille et al., <span>2013</span>). In 2013, she published <sup>142</sup>Nd/<sup>144</sup>Nd data for a 2.7 Ga basalt from Canada, Theo's Flow, the closest terrestrial analog for the nakhlite meteorites. Those rocks' <sup>142</sup>Nd/<sup>144</sup>Nd ratio is distinct from the Earth's nominal value, showing that early mantle inhomogeneities had not been erased by the time that basalt erupted. As with the nakhlites, the Nd isotope ratios in Theo's Flow constrain their planets' early mantle dynamics; for the early Earth, the implication is that the mantle did not convect vigorously. (I contributed slightly to that paper, as the source of the Theo's Flow samples.) Dr. Debaille and Craig O'Neill followed up the next year with a “review” paper (O'Neill &amp; Debaille, <span>2014</span>) which showed that the Earth's tectonics in the Hadean eon was mostly in stagnant-lid regimes with limited periods of more mobile crust.</p><p>Dr. Debaille has been on the continent of Antarctica five times, once with Ansmet and four times to the Belgian base, Princess Elisabeth station. The main goal of those expeditions was to collect meteorites on blue ice fields. This included camping on ice and snow, and keeping the focus on the potential meteorites in this magnificent but unforgiving landscape. She not only brought her expertise to these expeditions, but also her leadership to keep the team around her focused and in good spirits. Beyond the meteorites, the Belgian teams also tried to understand the concentration mechanism of meteorites at some specific places by collecting ice samples. In addition, the teams collected sediments for recovering micrometeorites around the Belgian station. Back at home, she is interested in the curation of the retrieved meteorites and how to ensure they are kept in good conditions in the museum to be available to worldwide scientists.</p><p>It was those curational skills, combined with her primary research that brought her onto the Measurement Definition Team for Mars Sample Return (Bridges &amp; Debaille, <span>2024</span>) an interest in Mars Sample Return we have shared since our LPI days (Beaty et al., <span>2019</span>). 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Her work has also been recognized by receipt of significant grants, including in 2014, an ERC starting grant, “Initial Starting Composition of the Solar System”; an Excellence of Science consortium grant “<i>Evolution and Tracers of the Habitability of Mars and Ancient Earth</i>”; and support to join the Mars 2020 Perseverance rover team as a Returned Sample Scientist and SuperCam team member. She was elected a fellow of our Meteoritical Society in 2024, and of course was the host in Brussels of last year's Annual meeting. With the Jessberger Award, we now add to the Society's recognition and honor for Dr. Debaille.</p><p>Ms. President, officers, council, and members of the Meteoritical Society, fellow scientists and guests, I present to you for the 2025 Jessberger Award: Professor Vinciane Debaille.</p>","PeriodicalId":18555,"journal":{"name":"Meteoritics & Planetary Science","volume":"60 S1","pages":"353-355"},"PeriodicalIF":2.4000,"publicationDate":"2025-07-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/maps.70011","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Meteoritics & Planetary Science","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/maps.70011","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Prof. Vinciane Debaille is the 2025 Jessberger awardee.

Back in 2020, a group of us, who had first met at the Lunar and Planetary Institute in Houston, reunited through the only means possible at the time: online. It not only bridged the geographic gap, but it also led us to reminisce about how much time had elapsed since we could sit around a table—usually also involving food—and chat in person. It was then that we remarked on how Vinciane had progressed, how she had developed from the postdoc we shared the table with in Houston to a world-leading researcher and professor of Isotope Geochemistry at Université de Libre Bruxelles in Belgium. We are delighted today that our colleagues share our judgment and that Vinciane will receive the 2025 Jessberger Award.

She then discovered that other planetary bodies have basalts, too, and need isotope geochemists! This is when she came to Houston in 2005 as a postdoc, working with Dr. Alan Brandon at NASA JSC to learn about (among others) extinct radioisotope chronometry and geochemistry. That collaboration led to three foundational papers that demonstrated Dr. Debaille's analytical prowess, her ability to make sense of complementary short- and long-lived isotope systems, and her skill at presenting elegant and understandable interpretations. Those three laid the foundation for her hugely successful career in meteorite and planetary sciences.

The first paper from her post-doctoral work, published in Nature (Debaille et al., 2007) in 2007, used high-precision analyses of the 142Nd/144Nd and 143Nd/144Nd ratios of shergottite martian meteorite to show that Mars likely experienced differentiation through progressive crystallization of a magma ocean within about 100 million years of core formation.

The second paper, in 2008 in Earth and Planetary Science Letters (Debaille et al., 2008), added 176Hf/177Hf data to the shergottite Nd story. There, she showed that the shergottites developed from mixtures of material enriched and depleted in incompatible trace elements, and implicated garnet fractionation in their sources.

The third of these seminal papers, 2009 in Nature Geoscience (Debaille et al., 2009), attacked the other martian meteorites, the nakhlites. From their isotopic systematics, short- and long-lived, Dr. Debaille inferred an early overturn of the martian mantle. These three papers have become the background, the environment, for all subsequent studies of Mars' early evolution.

After her enormously successful time in Houston, Dr. Debaille returned to Belgium to the Université Libre de Bruxelles, first as a postdoc and then to her current position as Senior Research Associate (Maître de recherche). In Brussels, she has continued her work on the isotopic characteristics of both meteorites and terrestrial systems, many in collaboration with students—at least 14 doctoral and 18 masters. Her works are far too numerous to read out here; they extend from familiar planetary and meteorite subjects to less-expected topics like non-traditional isotopes (like Fe and Zn), Fe–Ti ore deposits, banded iron formations, archaean granitoids, and blue ice.

Among Dr. Debaille's papers, one in particular (special to me) connects the terrestrial and planetary realms (Debaille et al., 2013). In 2013, she published 142Nd/144Nd data for a 2.7 Ga basalt from Canada, Theo's Flow, the closest terrestrial analog for the nakhlite meteorites. Those rocks' 142Nd/144Nd ratio is distinct from the Earth's nominal value, showing that early mantle inhomogeneities had not been erased by the time that basalt erupted. As with the nakhlites, the Nd isotope ratios in Theo's Flow constrain their planets' early mantle dynamics; for the early Earth, the implication is that the mantle did not convect vigorously. (I contributed slightly to that paper, as the source of the Theo's Flow samples.) Dr. Debaille and Craig O'Neill followed up the next year with a “review” paper (O'Neill & Debaille, 2014) which showed that the Earth's tectonics in the Hadean eon was mostly in stagnant-lid regimes with limited periods of more mobile crust.

Dr. Debaille has been on the continent of Antarctica five times, once with Ansmet and four times to the Belgian base, Princess Elisabeth station. The main goal of those expeditions was to collect meteorites on blue ice fields. This included camping on ice and snow, and keeping the focus on the potential meteorites in this magnificent but unforgiving landscape. She not only brought her expertise to these expeditions, but also her leadership to keep the team around her focused and in good spirits. Beyond the meteorites, the Belgian teams also tried to understand the concentration mechanism of meteorites at some specific places by collecting ice samples. In addition, the teams collected sediments for recovering micrometeorites around the Belgian station. Back at home, she is interested in the curation of the retrieved meteorites and how to ensure they are kept in good conditions in the museum to be available to worldwide scientists.

It was those curational skills, combined with her primary research that brought her onto the Measurement Definition Team for Mars Sample Return (Bridges & Debaille, 2024) an interest in Mars Sample Return we have shared since our LPI days (Beaty et al., 2019). Dr. Debaille's contributions to this community effort to maximize the scientific return of those precious samples when they arrive here on Earth are fundamental, numerous, and always insightful. She has been instrumental in optimizing our thinking and preparation for the arrival of Martian samples here on Earth—and their studies for centuries to come.

Dr. Debaille's expertise and scientific contributions have been widely recognized, both by prizes and by grant fundings. In 2012, she received the Baron van Ertborn Prize of the Royal Academy of Belgium for her work in geology, isotope geochemistry and planetary science. In 2014, she was the first recipient of the “Atomia” Prize for her work on understanding early Earth, awarded to a young female scientist by the Brussels' Ministry for Scientific Research. Her work has also been recognized by receipt of significant grants, including in 2014, an ERC starting grant, “Initial Starting Composition of the Solar System”; an Excellence of Science consortium grant “Evolution and Tracers of the Habitability of Mars and Ancient Earth”; and support to join the Mars 2020 Perseverance rover team as a Returned Sample Scientist and SuperCam team member. She was elected a fellow of our Meteoritical Society in 2024, and of course was the host in Brussels of last year's Annual meeting. With the Jessberger Award, we now add to the Society's recognition and honor for Dr. Debaille.

Ms. President, officers, council, and members of the Meteoritical Society, fellow scientists and guests, I present to you for the 2025 Jessberger Award: Professor Vinciane Debaille.

Abstract Image

2025年杰斯伯格奖:Vinciane Debaille教授
文西安·德巴耶教授是2025年杰斯伯格奖获得者。早在2020年,我们一群人第一次在休斯顿的月球和行星研究所见面,通过当时唯一可能的手段重聚:网上。它不仅弥合了地理上的鸿沟,而且还让我们回忆起自从我们能够围坐在一张桌子旁——通常还有食物——面对面聊天以来,已经过去了多少时间。就在那时,我们谈到了文西安的进步,她是如何从我们在休斯顿同桌的博士后,成长为比利时布鲁塞尔自由大学(universit<s:1> de Libre Bruxelles)世界一流的研究员和同位素地球化学教授的。今天,我们很高兴我们的同事们同意我们的判断,文西安将获得2025年杰斯伯格奖。然后她发现其他行星体也有玄武岩,并且需要同位素地球化学家!2005年,她作为博士后来到休斯敦,与NASA JSC的艾伦·布兰登博士一起学习(以及其他)已灭绝的放射性同位素计时和地球化学。在那次合作中,德巴耶发表了三篇基础论文,展示了她的分析能力、她对互补的短寿命和长寿命同位素系统的理解能力,以及她提出优雅而易懂的解释的技巧。这三件事为她在陨石和行星科学领域取得巨大成功奠定了基础。她博士后工作的第一篇论文于2007年发表在《自然》杂志上(Debaille et al., 2007),通过对火星陨石的142 /144Nd和143Nd/144Nd比率的高精度分析,表明火星可能在岩心形成约1亿年的时间里,通过岩浆海洋的逐步结晶经历了分化。第二篇论文发表在2008年的《地球与行星科学快报》(Debaille et al., 2008)上,将176Hf/177Hf的数据添加到长石Nd的故事中。在那里,她证明了这些辉高石是由富含和缺乏不相容微量元素的物质混合而成的,并且暗示了它们来源中的石榴石分馏。第三篇开创性论文发表于2009年的《自然地球科学》(Debaille et al., 2009),攻击了另一种火星陨石——nakhlites。根据他们的同位素系统,短期和长期存在,德巴耶博士推断出火星地幔的早期翻转。这三篇论文成为后来所有关于火星早期演化的研究的背景和环境。在休斯顿取得巨大成功后,德巴耶博士回到比利时布鲁塞尔自由大学,先是博士后,然后担任高级研究助理(matre de recherche)。在布鲁塞尔,她继续研究陨石和陆地系统的同位素特征,其中许多是与学生合作的,其中至少有14名博士和18名硕士。她的作品太多了,无法在这里一一阅读;它们从熟悉的行星和陨石主题延伸到不太令人期待的主题,如非传统同位素(如铁和锌)、铁钛矿床、带状铁地层、太古代花岗岩类和蓝冰。在Debaille博士的论文中,有一篇特别(对我来说特别)将地球和行星领域联系起来(Debaille et al., 2013)。2013年,她发表了来自加拿大的2.7 Ga玄武岩的142 /144Nd数据,Theo's Flow是最接近nakhlite陨石的陆地模拟物。这些岩石的142 /144Nd比值与地球的标称值不同,表明玄武岩喷发时,早期地幔的不均匀性并未被消除。与纳克里岩一样,西奥流中的Nd同位素比率限制了它们行星的早期地幔动力学;对于早期地球来说,这意味着地幔没有强烈的对流。(作为Theo’s Flow样本的来源,我对那篇论文做出了些许贡献。)德巴耶博士和克雷格·奥尼尔(Craig O'Neill)在第二年发表了一篇“综述”论文(O'Neill &; Debaille, 2014),该论文表明,冥古宙的地球构造大部分处于停滞状态,地壳的活动期有限。德巴耶已经五次来到南极洲,一次是和安斯梅特一起,四次是到比利时基地伊丽莎白公主站。这些探险的主要目标是收集蓝色冰原上的陨石。这包括在冰雪上露营,并将注意力集中在这片壮丽但无情的景观中潜在的陨石上。她不仅把自己的专业知识带到了这些探险中,而且还把她的领导能力带到了她周围的团队,让她保持专注和良好的精神状态。除了陨石,比利时团队还试图通过收集冰样本来了解陨石在某些特定地点的集中机制。此外,这些小组还收集了沉积物,以便在比利时站周围回收微陨石。 回到家后,她对取回的陨石的管理以及如何确保它们在博物馆中保持良好的状态以供世界各地的科学家使用感兴趣。正是这些管理技能,加上她的主要研究,使她加入了火星样本返回的测量定义团队(Bridges & Debaille, 2024年),我们从LPI时代起就对火星样本返回感兴趣(Beaty等人,2019年)。当这些珍贵的样本到达地球时,德巴耶博士为最大限度地提高它们的科学回报所做的贡献是基础性的、大量的,而且总是有见地的。她在优化我们的思考和准备火星样本抵达地球以及未来几个世纪的研究方面发挥了重要作用。德巴耶的专业知识和科学贡献得到了广泛的认可,无论是奖项还是资助。2012年,她因在地质学、同位素地球化学和行星科学方面的工作而获得比利时皇家科学院的范·厄特恩男爵奖。2014年,她因在了解早期地球方面的工作而成为第一位获得“原子”奖的人,该奖项由布鲁塞尔科学研究部颁发给一位年轻的女科学家。她的工作也得到了重要资助的认可,包括2014年的ERC启动资助,“太阳系的初始起始成分”;卓越科学联盟资助“火星和古代地球宜居性的进化和示踪剂”;并支持作为返回样本科学家和超级相机团队成员加入2020年火星毅力号火星车团队。她在2024年被选为我们气象学会的会员,当然,她还是去年在布鲁塞尔召开的年会的主持人。有了Jessberger奖,我们现在增加了协会对debaille博士的认可和荣誉。主席,官员们,理事会,气象学会的成员们,科学家们的同事们,来宾们,我向你们推荐2025年杰斯伯格奖的得主:文西安·德巴耶教授。
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来源期刊
Meteoritics & Planetary Science
Meteoritics & Planetary Science 地学天文-地球化学与地球物理
CiteScore
3.90
自引率
31.80%
发文量
121
审稿时长
3 months
期刊介绍: First issued in 1953, the journal publishes research articles describing the latest results of new studies, invited reviews of major topics in planetary science, editorials on issues of current interest in the field, and book reviews. The publications are original, not considered for publication elsewhere, and undergo peer-review. The topics include the origin and history of the solar system, planets and natural satellites, interplanetary dust and interstellar medium, lunar samples, meteors, and meteorites, asteroids, comets, craters, and tektites. Our authors and editors are professional scientists representing numerous disciplines, including astronomy, astrophysics, physics, geophysics, chemistry, isotope geochemistry, mineralogy, earth science, geology, and biology. MAPS has subscribers in over 40 countries. Fifty percent of MAPS'' readers are based outside the USA. The journal is available in hard copy and online.
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