
國立中山大學研究團隊發現,沿海生態系統產生的藍碳可經由洋流運送超過1000公里至西北太平洋低緯度暖池區深海,成為深海碳匯。研究利用環境DNA和穩定碳同位素技術識別藻類、紅樹林和海藻的生物信號,發現其在500至1000米深度的有機碳通量比傳統模型預測高2.7至4.2倍,顯示傳統垂直沉降模型無法完全解釋深海碳通量機制。此研究主要由國家科技委員會「航向藍海」計畫資助。
AI-generated summary
過去研究多聚焦於海洋表層生物碳的垂直下通量,但本研究證明藍碳可經由洋流水平輸送至遠離陸地的深海區域,挑戰傳統碳通量模型。
《TAIPEI TIMES》 Deep-ocean carbon trails tracked
Members of a research team from National Sun Yat-sen University pose for a photograph on the research vessel Legendin the northwestern Pacific in an undated photograph. Photo courtesy of National Sun Yat-sen University
By Esme Yeh / Staff reporter
“Blue carbon” produced by coastal ecosystems might “ride” ocean currents for more than 1,000km to fuel deep-ocean carbon sinks, National Sun Yat-sen University researchers said on Thursday.
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The university’s Carbon Research Lab, led by Hung Chin-chang (洪慶章), a professor of oceanography, conducted oceanographic observations in the low-latitude warm pool of the northwestern Pacific, an area often called an “ocean desert” due to low biological productivity and a lack of nutrients.
Researchers detected biosignals of algae, mangroves and seaweed at depths of 500m to 1,000m in the area, Hung said.
The results showed that organic matter produced in coastal systems can be carried by ocean circulation systems into the deep sea far from land, the university said in a statement.
The research is primarily funded by the “sailing to the blue sea” project of the the National Science and Technology Council, it said.
The research team on the research vessel Legend in 2023 visited five oceanographic stations in the northwestern Pacific, where they conducted observations, it said.
Drifting sediment traps were deployed in waters at depths of 150m, 500m and 1,000m around the stations to collect sinking organic particles, the statement said.
Stable carbon isotopes from the samples were used to distinguish between land-derived and ocean-derived sources, while environmental DNA (eDNA) was used to identify the organisms from which the carbon originated, it said.
The results showed that eDNA signals of large algae, mangroves and seaweed were detected at depths of 500m and 1,000m, it said.
The five oceanographic stations spanned four degrees of latitude, with some of them about 900km from the Philippines and more than 1,200km from Indonesia, the university said.
However, eDNA and isotope evidence is insufficient to determine whether the blue carbon originated from Palau, the Philippines or Indonesia, it said.
Mangroves, seaweed beds and algae are important coastal blue carbon ecosystems that can absorb carbon dioxide and store it in their biomass and surrounding environment, the university said.
While previous studies mostly focused on marine biological carbon’s downward flux from the ocean surface, the university’s research showed that carbon can travel via currents to the open ocean — a carbon transport pathway that has not received much research attention, it said.
The research is significant, as it provides evidence showing that carbon sequestrated by coastal systems can reach the deep ocean, it said.
Surface currents, submarine currents and mesoscale eddies all contribute to the transportation processes, it added.
The research showed that carbon in the ocean can float a long way out to sea before sinking, the university said.
The particulate organic carbon flux measured at 1,000m were 2.7 to 4.2 times higher than the values predicted with the Martin Curve carbon attenuation model, it said.
That shows that the conventional vertical sinking model might not fully explain the carbon flux mechanism in the deep ocean, the university added.
新聞來源:TAIPEI TIMES
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AI outlook — possibilities, not facts
未來研究將針對藍碳具體來源國進行更精準的追蹤
Likely · Within months
此發現將促使修訂現有的海洋碳通量模型,納入水平輸送過程
Likely · Within months

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