在托尔西安无氧事件中,海洋酸化被石灰泥记录中的同位素所捕获
Simone A Kasemann1, Tina Klein1, Richard A Boyle2
1Faculty of Geosciences and MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.
概括
托尔西亚海洋无氧事件导致海洋酸化,但只有石灰泥,而不是贝,记录了这种pH值变化. 这表明一些海洋生物可以缓冲这些环境变化.
科学领域:
- 古海洋学是古海洋学.
- 地质化学 地质化学
- 气候科学 气候科学
背景情况:
- 托尔西亚海洋无氧事件 (大约. 183亿年前) 是一个与气候和海洋循环变化相关的全球大规模灭绝时期.
- 大型火山活动可能会释放二氧化碳,导致变暖,脱氧和酸化.
研究的目的:
- 为了量化在托尔西亚海洋无氧事件期间海洋酸化的程度.
- 评估不同海洋碳酸盐成分作为过去海洋pH记录器的可靠性.
主要方法:
- 分析了来自两个西南欧海洋区的微生物,足动物和双动物的同位素数据.
- 利用一个合的生物地化学模型来模拟海洋酸化.
主要成果:
- 来自微石的同位素数据显示了暂时的减少,这表明在事件期间海洋酸化.
- 臂足动物和双玻尿酸同位素值保持稳定,这表明生理pH缓冲.
- 模型模拟成功地重现了观察到的海洋酸化事件.
结论:
- 微是一种可靠的档案,用于跟踪过去的海洋pH值变化,即使是在快速事件期间.
- 两动物和足动物不太适合重建历史海洋pH值,因为它们有缓冲环境变化的能力.
- 托尔西亚海洋无氧事件引发了显著的,尽管是暂时的,海洋酸化.
更多相关视频
相关概念视频
Titration of Polyprotic Base with a Strong Acid
882
The titration of a polyprotic base such as sodium carbonate with a strong acid such as hydrochloric acid results in two equivalence points on the titration curve. At the first equivalence point, the carbonate ions in the base are completely converted to bicarbonate ions. The second equivalence point corresponds to the complete conversion of bicarbonate ions to carbonic acid, which dissociates into carbon dioxide and water. The region before the first equivalence point corresponds to the...
882
The Carbon Cycle
40.0K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
40.0K
The Fossil Record
25.7K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
25.7K
Bicarbonate-Carbonic Acid Buffer
3.2K
The carbonic acid-bicarbonate buffer system is critical for maintaining the body's pH balance. It operates on the equilibrium:
3.2K
Factors Affecting Solubility
33.9K
Compared with pure water, the solubility of an ionic compound is less in aqueous solutions containing a common ion (one also produced by dissolution of the ionic compound). This is an example of a phenomenon known as the common ion effect, which is a consequence of the law of mass action that may be explained using Le Chȃtelier’s principle. Consider the dissolution of silver iodide:
33.9K
The Phosphorus Cycle
38.9K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
38.9K


