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Making Time to Cultivate Our Interdisciplinary Curiosity 挤出时间培养我们的跨学科好奇心
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.263
Becky Lange
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引用次数: 0
International Association of Mineralogy 国际矿物学协会
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.309
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引用次数: 0
High-Precision Geochronology of LIP Intrusions: Records of Magma–Sediment Interaction LIP侵入体的高精度地质年代:岩浆-沉积相互作用的记录
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.302
S. Gaynor, Joshua Davies, U. Schaltegger
Reconstructing the tempo and emplacement mechanisms of large igneous provinces (LIPs) and establishing potential links to environmental change and biological crises requires detailed and targeted high-precision geochronology. Contact metamorphism during LIP intrusive magmatism can release large volumes of thermogenic gas, so determining the timing of these events relative to global climate change is crucial. The most reliable age information comes from U-Pb geochronology; however, LIP mafic igneous rocks do not commonly crystallize U-bearing minerals, such as zircon or baddeleyite. Recent work has shown that U-rich minerals can crystallize in fractionated melt pockets in intrusive components of LIPs after contamination of the melt by sedimentary rocks at emplacement level. Zircon and baddeleyite from these pockets make high-precision U-Pb geochronology of LIPs possible, but these unique mechanisms add other complexities.
要重建大型火成岩带(LIPs)的形成速度和成岩机制,并建立与环境变化和生物危机的潜在联系,需要详细而有针对性的高精度地质年代学。大火成岩带侵入岩浆作用期间的接触变质作用可释放出大量热成气体,因此确定这些事件与全球气候变化的时间关系至关重要。最可靠的年龄信息来自 U-Pb 地质年代学;然而,LIP 黑云母火成岩通常不会结晶出锆石或巴德磊石等含铀矿物。最近的研究表明,LIPs侵入成分中的熔体在成岩阶段受到沉积岩的污染后,可在分馏熔体袋中结晶出富铀矿物。这些熔块中的锆石和巴德磊石使得高精度的 LIPs U-Pb 地质年代成为可能,但这些独特的机制增加了其他复杂性。
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引用次数: 0
The Franklin Large Igneous Province and Snowball Earth Initiation 富兰克林大火成岩带与雪球地球的形成
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.296
Francis A. Macdonald, N. Swanson‐Hysell
Large igneous provinces (LIPs) can potentially cause cooling on tens- to thousand-year timescales via injection of sulfur aerosols to the tropo-sphere, and on million-year timescales due to the increase of global weatherability. The ca. 719-Ma Franklin LIP preceded onset of the Sturtian Snowball Earth glaciation by less than two million years, consistent with CO2 drawdown due to weathering of Ca- and Mg-rich LIP basalts, which may have contributed to cooling past a critical runaway ice-albedo threshold. A relatively cool background climate state and Franklin LIP emplacement near a continental margin in the warm wet tropics may have been critical factors for pushing the Earth’s climate past the threshold of runaway glaciation.
大火成岩带(LIPs)通过向三极球注入硫气溶胶,有可能在万年到千年的时间尺度上造成降温,而由于全球可变性的增加,则有可能在百万年的时间尺度上造成降温。约约 719-Ma 富兰克林 LIP 比斯图尔特雪球地球冰川期开始早不到 200 万年,这与富含钙和镁的 LIP 玄武岩风化导致的二氧化碳减少是一致的,这可能导致冷却超过了冰-冰床失控的临界阈值。相对凉爽的背景气候状态和富兰克林LIP在暖湿热带地区大陆边缘附近的隆起可能是推动地球气候越过冰川失控临界点的关键因素。
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引用次数: 0
Meet Linkedin’s Popular Geo-Blogger 认识 Linkedin 最受欢迎的地理博客作者
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.330
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引用次数: 0
Whole Earth Controls on the Evolution of Life 整个地球对生命进化的控制
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.267
Cin-Ty Lee
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引用次数: 0
Industry 4.0—in the Middle of the Transformation 工业 4.0--转型的中间环节
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.331
Uwe König
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引用次数: 0
How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times 大型火成岩带如何杀死地球上的大多数生命--无数次
IF 4.5 2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-01 DOI: 10.2138/gselements.19.5.276
S. Grasby, D. P. Bond
Evolution has not been a simple path. Since the first appearance of complex life, there have been several mass extinctions on Earth. This was exemplified by the most severe event during the Phanerozoic, the end-Permian mass extinction that occurred 252 million years ago and saw a loss of 90% and 70% of all marine and terrestrial species, respectively. Such mass extinctions have entirely reset ecosystems. Increasing evidence points to the massive eruption and crustal emplacement of magmas associated with large igneous provinces (LIPs) as key drivers of these events. Understanding how LIP events disrupted global biogeochemical cycles is of prime importance, especially as humans alter the atmosphere and biosphere today. We explore the cascading impacts of LIP events on global climate, oceans, and land—including runaway greenhouses, the release of toxic metals to the environment, the destruction of the ozone layer, and how global oceans are driven to anoxic and acidic states—all of which have parallels in the consequences of modern industrialisation.
进化并非一条简单的道路。自复杂生命首次出现以来,地球上已发生过数次生物大灭绝。其中最严重的一次是发生在 2.52 亿年前的新生代时期,即二叠纪末期的大灭绝,海洋和陆地物种分别减少了 90% 和 70%。这种大灭绝完全重置了生态系统。越来越多的证据表明,与大火成岩带(LIPs)相关的岩浆的大规模喷发和地壳置换是这些事件的关键驱动因素。了解大火成岩带事件如何破坏全球生物地球化学循环至关重要,尤其是在人类改变大气层和生物圈的今天。我们探讨了大火成岩带事件对全球气候、海洋和陆地的连锁影响,包括温室失控、有毒金属向环境释放、臭氧层破坏以及全球海洋如何被推向缺氧和酸性状态--所有这些都与现代工业化的后果相似。
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引用次数: 0
International Association of GeoChemistry 国际地球化学协会
2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-01 DOI: 10.2138/gselements.19.4.244
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引用次数: 0
Mineralogical Society of America 美国矿物学学会
2区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-01 DOI: 10.2138/gselements.19.4.242
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引用次数: 0
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