グローバルな植物プランクトンの減少は,過去100年にわたって続いている
Daniel G Boyce1, Marlon R Lewis, Boris Worm
1Biology Department, Dalhousie University, Halifax, Nova Scotia, Canada, B3H 4J1. dboyce@dal.ca
Nature
|July 31, 2010
まとめ
グローバルな植物プランクトン濃度は,1899年以来,毎年約1%減少しており,海洋生態系に影響を与えています. 海洋温度の上昇と結びついたこの1世紀に渡る傾向は,短期的な気候変動による変動と対照的です.
科学分野:
- マリン・バイオロジー マリン・バイオロジー
- 海洋学 海洋学とは
- 気候科学 気候科学
背景:
- 植物プランクトンは,地球の有機物質生産の約半分を担う重要な海洋光栄養生物です.
- 過去の衛星データ (1979年以来) は,数十年間の変動を示したが,長期の傾向を示すのに十分な長さがなかった.
研究 の 目的:
- 1899年から現在までの植物プランクトンバイオマストレンドを,地域,地域,そして地球規模で再構築し,分析する.
- 観察された植物プランクトンの変動と長期的な変化の要因を調査する.
主な方法:
- 歴史的な海洋透明度測定とインシットクロロフィルの観測を組み合わせた.
- 統計的方法を使用して,時間に依存する植物プランクトンバイオマスを分析しました.
主要な成果:
- 研究された10の海洋地域のうち8のフィトプランクトン濃度の減少が観察されました.
- 推定の世界平均減少率は,年間約1%である.
- 年間間/十年間変動と気候指数,そして長期の傾向と海面温度上昇との間の相関を特定した.
結論:
- グローバルな植物プランクトン濃度は,過去100年にわたって著しく減少しています.
- 海面温度の上昇は,観測された長期的減少の重要な要因である.
- この"世紀に渡る衰退は,将来の海洋生態系,地化学,漁業の研究で考慮する必要がある.
関連する概念動画
Primary Production
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
Global Climate Change
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.
Threats to Biodiversity
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...
Conservation of Declining Populations
Conservation of declining population focuses on ways of detecting, diagnosing, and halting a population decline. The approach uses methods to prevent populations from going extinct.
Marine Microbial Ecology
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Freshwater Microbial Ecology
Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic systems...


