碳同位素预算表明,在最后的冰川最大期,生物不平衡主导了海洋碳储存
Anne Willem Omta1, Christopher L Follett2,3, Jonathan M Lauderdale3
1Department of Earth, Environmental, and Planetary Sciences, Case Western Reserve University, Cleveland, OH, USA. anne.omta@case.edu.
Nature communications
|September 12, 2024
概括
海洋碳储存变化解释了冰河时代和温暖时期之间的大气二氧化碳主要转移. 这种由海冰或循环变化驱动的生物碳不平衡是了解过去气候变化的关键.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 大气中的二氧化碳水平在冰川和冰川间时期之间波动了90ppmv.
- 地球系统模型需要多个过程来解释这些二氧化碳波动.
- 循环的规律性表明主要的驱动机制.
研究的目的:
- 量化生物隔离海洋碳在冰川和冰川间大气二氧化碳变化中的作用.
- 研究海洋碳储存变化背后的机制.
主要方法:
- 使用公布的碳同位素测量结果进行质量平衡计算.
- 在不同海洋水体中分析碳同位素特征.
主要成果:
- 生物隔离的海洋碳可以占大气二氧化碳变化的75±40 ppmv.
- 在最后的冰川最大期和全新纪期间,再生碳库存类似.
- 碳储存的变化主要是由不平衡,而不是库存转移.
结论:
- 海洋碳不平衡是冰川和冰川间大气二氧化碳波动的主要驱动因素.
- 海冰的膨胀或海洋翻转循环的变化可能导致了这种不平衡.
相关概念视频
Global Climate Change
24.3K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.3K
The Carbon Cycle
37.1K
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.
37.1K
What are Biogeochemical Cycles?
31.2K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
31.2K
The Fossil Record
25.1K
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...
25.1K
Threats to Biodiversity
22.2K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.2K
Carbon Dioxide Transport in the Blood
1.7K
Carbon dioxide (CO2) transport in the blood is critical to human physiology. On average, our body cells produce around 200 mL of CO2 per minute, precisely the quantity expelled by the lungs. This process involves the transportation of CO2 from the tissue cells to the lungs in three primary forms.
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
1.7K


