Elemental-organic geochemical evidence for the lacustrine metalimnetic oxygen minimum dynamics in the Mid-Late Triassic Chang 7 shales DOI
Leibo Bian, Xiaomei Wang, Anthony Chappaz

et al.

Earth and Planetary Science Letters, Journal Year: 2024, Volume and Issue: 651, P. 119153 - 119153

Published: Dec. 2, 2024

Language: Английский

New advances in the study of Tethyan Geodynamic System DOI
Lin Ding

Science China Earth Sciences, Journal Year: 2024, Volume and Issue: 67(3), P. 874 - 878

Published: Feb. 23, 2024

Language: Английский

Citations

6
The impact of ocean acidification on gastropod shell dissolution and microstructure DOI
Xing Li, Haijun Song, Li Tian

et al.

Anthropocene, Journal Year: 2025, Volume and Issue: unknown, P. 100470 - 100470

Published: March 1, 2025

Language: Английский

Citations

0
Impact of Tethyan domain evolution on the formation of petroleum systems in the Sichuan super basin, SW China DOI Creative Commons

Shuyuan Shi,

Wei Yang, Gang Zhou

et al.

Petroleum Exploration and Development, Journal Year: 2024, Volume and Issue: 51(5), P. 1183 - 1201

Published: Oct. 1, 2024

Language: Английский

Citations

3
The relation between the Givetian and Serpukhovian biotic crises and long-term environmental trend changes DOI Creative Commons
Dmitry A. Ruban

Geosystems and Geoenvironment, Journal Year: 2024, Volume and Issue: 3(2), P. 100265 - 100265

Published: Feb. 24, 2024

Explanations for major catastrophes in the history of life commonly focus on their time-spans. Less biotic crises are worth attention as well, however, which requires investigation a longer-lasting context. The present study relates Taghanic (Givetian) and mid-Carboniferous (Serpukhovian) to some long-term changes environmental developments. trends these developments interpreted basis global sea level, average temperatures, total surface area exposed land, number lithospheric plates, concentration atmospheric oxygen. It is found that can be related directly or indirectly changes.

Language: Английский

Citations

0
重建深时地球生物多样性时空分布模式的思考 DOI Creative Commons
Shuhan Zhang, Shu‐zhong Shen, Xiangdong Wang

et al.

Chinese Science Bulletin (Chinese Version), Journal Year: 2024, Volume and Issue: 69(22), P. 3252 - 3267

Published: April 30, 2024

重建地球生物多样性演变历史是了解地球生命演化规律的关键。通过研究地质时期的生物多样性变化,能够追溯生命的起源、演化和灭绝过程,并探索其原因。然而,地球上曾经生活过的99%以上的生物都已经被替代,其中只有一小部分保存为化石并被人类发现。因此,如何利用化石记录重建地球生物多样性变化的过程是一个非常复杂的科学难题,为了解决这一难题,我们需要从多方面入手。首先,建立含有时空信息的全球性大型综合数据库是研究深时生物多样性模式的必要条件,也是识别曾经发生过的重大生物事件的基础,以往的研究多集中在海洋无脊椎动物化石多样性的研究,目前仍然缺乏全球性的陆地生物多样性模式。其次,需要解决化石保存不完整和样本采集时空不均一的难题。近十几年来,随着海量数据的积累,大数据分析技术的发展,通过多学科交叉,在解决时空分辨率低和样本偏差等问题上发展了更有效的分析手段,但仍然任重道远。第三,新的大数据研究结果引发了对深时地球生物多样性变化的时空规律的许多新认识。随着研究的深入,五次生物大灭绝的灭绝幅度和灭绝率明显降低,需要以全球大数据为基础重新精确估算,其中二叠纪末生物大灭绝无疑仍是最大的一次,而泥盆纪晚期F/F和三叠纪末灭绝事件很可能算不上五大生物灭绝之二,白垩纪末生物大灭绝的持续时间和灭绝幅度也需要重新估算。此外,寒武纪-奥陶纪、石炭纪-二叠纪和新生代三大生物辐射也需要全球高分辨率化石数据验证。以人工智能和超级计算机等为手段建立的深时生态系统演变模型是实现古今对比的未来方向,这些研究将使我们对地球生物多样性历史有全方位的认识,也为现今的全球生态系统面临的问题提供深时参照。

Citations

0
Gigantic gastropods from the Middle Triassic Qingyan biota of Guizhou DOI
Xin Sun, Li Tian,

Chuan-Yuan Liu

et al.

Palaeoworld, Journal Year: 2024, Volume and Issue: 33(5), P. 1425 - 1434

Published: May 14, 2024

Language: Английский

Citations

0
Elemental-organic geochemical evidence for the lacustrine metalimnetic oxygen minimum dynamics in the Mid-Late Triassic Chang 7 shales DOI
Leibo Bian, Xiaomei Wang, Anthony Chappaz

et al.

Earth and Planetary Science Letters, Journal Year: 2024, Volume and Issue: 651, P. 119153 - 119153

Published: Dec. 2, 2024

Language: Английский

Citations

0