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A
Abigail McQuatters-Gollop
C
Carol Robinson
C
Christopher Lowe
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Abigail McQuatters-Gollop: 浮游生物种类繁多,分为植物性浮游生物(藻类)和动物性浮游生物(微小动物)。许多动物性浮游生物是其他海洋动物的幼体阶段,形态各异。它们无法逆流而动,只能随波逐流,因此被称为浮游生物。持续浮游生物记录调查(CPR)为研究浮游生物提供了长期、大范围的数据。气候变化导致海水温度升高,改变了浮游生物的地理分布,对海洋食物网产生影响,例如,暖水浮游生物取代冷水浮游生物,影响以浮游生物为食的鱼类,如鳕鱼的幼体。人类活动,例如营养物质过量排放,会导致藻华,消耗水体氧气,形成死区,危害海洋生物。 Christopher Lowe: 浮游生物大小差异巨大,从肉眼不可见的单细胞细菌到大型水母,大小相差悬殊。虽然许多浮游生物肉眼不可见,但它们的数量巨大,足以改变水体的颜色,甚至可以从太空观测到。植物性浮游生物的光合作用对地球早期大气氧气的产生至关重要,海洋中植物性浮游生物的演化方式与陆地植物不同,存在多种不同的光合作用途径。混合营养型浮游生物兼具自养和异养特性,既能进行光合作用,也能捕食其他浮游生物。航运活动通过船体附着生物和压载水等途径,导致浮游生物的迁移和入侵,改变了浮游生物的地理分布。 Carol Robinson: 生物碳泵通过一系列物理和生物过程将大气中的二氧化碳转移到深海或沉积物中,对调节大气二氧化碳浓度至关重要。动物性浮游生物的昼夜垂直迁移是生物碳泵的重要组成部分,它能加速碳从表层水体向深层水体的运输。海水温度升高会影响浮游生物的光合作用和呼吸作用,降低生物碳泵的效率,加剧气候变化。海洋酸化会影响浮游生物的生长和钙化作用,改变生物碳泵的效率。浮游生物的生长需要多种营养物质,这些营养物质的来源包括河流、陆地径流、大气沉降等。目前尚无法确定通过人为干预来增强海洋碳汇的有效性和安全性,需要开展更多研究。

Deep Dive

Key Insights

What is the significance of phytoplankton in Earth's history?

Phytoplankton played a crucial role in Earth's development by producing oxygen through photosynthesis. Around 2.4 billion years ago, they began oxygenating the atmosphere, which was previously devoid of oxygen. This process allowed life as we know it to emerge. Today, phytoplankton contribute to about half of the oxygen we breathe.

What is the biological carbon pump and how does it work?

The biological carbon pump is a process that moves carbon dioxide from the atmosphere into the deep ocean, where it is stored. Phytoplankton photosynthesize at the surface, taking up carbon dioxide. When they die or are eaten by zooplankton, their remains sink as marine snow. This carbon is respired by deep-sea organisms, trapping it in the ocean for hundreds of years. Without this pump, atmospheric carbon dioxide levels would be 30% higher.

How do zooplankton contribute to the carbon cycle?

Zooplankton play a key role in the carbon cycle by feeding on phytoplankton at the surface and then migrating to deeper waters during the day to avoid predators. They excrete and defecate at depth, transporting carbon quickly to the ocean floor. This process, known as the 'greatest migration on Earth,' helps sequester carbon in the deep ocean.

What is the Continuous Plankton Recorder Survey and why is it important?

The Continuous Plankton Recorder (CPR) Survey, started in 1931, is a long-term monitoring program that collects plankton samples from oceans worldwide. Using a simple device towed by ships, it captures plankton on silk, providing a consistent and extensive dataset. This survey has revealed changes in plankton communities due to climate change and other human impacts, offering critical insights into marine ecosystems.

How does ocean acidification affect plankton?

Ocean acidification, caused by increased carbon dioxide dissolving in seawater, lowers pH and reduces carbonate ion concentration. This makes it harder for plankton like coccolithophores and sea butterflies to produce calcium carbonate shells. While some phytoplankton benefit from higher carbon dioxide levels for photosynthesis, others struggle to maintain their protective structures, affecting their survival and the efficiency of the biological carbon pump.

What are mixotropes and how do they differ from other plankton?

Mixotropes are plankton that can both photosynthesize like phytoplankton and hunt like zooplankton. They switch between these modes depending on light and nutrient availability. This adaptability allows them to thrive in diverse environments, filling ecological niches that other plankton cannot. Some mixotropes, like dinoflagellates, are also responsible for bioluminescence in coastal waters.

How do human activities impact plankton distribution?

Human activities, such as shipping and the construction of canals, have significantly impacted plankton distribution. Ships transport plankton either through ballast water or by carrying organisms on their hulls, introducing invasive species to new regions. Infrastructure like the Panama and Suez Canals connects previously isolated ocean basins, allowing plankton to spread and disrupt local ecosystems.

What happens when nutrient balances in the ocean are disrupted?

Disruptions in nutrient balances, often caused by human activities like farming and sewage discharge, can lead to phytoplankton blooms. These blooms deplete oxygen as they decay, creating dead zones where marine life cannot survive. For example, the Black Sea experienced severe oxygen depletion in the 1980s due to excessive nutrients from rivers, leading to mass die-offs of benthic organisms.

How does temperature change affect plankton?

Rising temperatures affect plankton in multiple ways. Warmer waters increase the rates of photosynthesis and respiration, but respiration increases more, reducing the efficiency of the biological carbon pump. Temperature changes also alter nutrient availability and habitat conditions, impacting plankton distribution. For example, in the Antarctic, reduced sea ice has led to declines in phytoplankton, affecting the entire food web, including krill, penguins, and seals.

What would happen if plankton disappeared?

If plankton disappeared, Earth's ecosystems would collapse. Phytoplankton produce 50% of the oxygen we breathe, and they form the base of the marine food web, supporting everything from small fish to whales. Without plankton, marine life would dwindle, and the planet's atmosphere would become uninhabitable. Plankton are essential for maintaining the balance of life on Earth.

Chapters
Plankton are diverse, drifting organisms crucial to the marine food chain and Earth's oxygen production. They are categorized into phytoplankton (plant-like) and zooplankton (animal-like), exhibiting a vast range of sizes and shapes. Their significance is highlighted through their role in oxygen generation and the marine ecosystem.
  • Plankton are categorized into phytoplankton and zooplankton.
  • Half of the oxygen we breathe comes from plankton.
  • Plankton's daily migration is the largest migration of life on Earth.
  • Plankton's diversity in shapes and sizes is vast.
  • Plankton are observed through changes in water color, even from space.

Shownotes Transcript

Melvyn Bragg and guests discuss the tiny drifting organisms in the oceans that sustain the food chain for all the lifeforms in the water and so for the billions of people who, in turn, depend on the seas for their diet. In Earth's development, the plant-like ones among them, the phytoplankton, produced so much oxygen through photosynthesis that around half the oxygen we breathe today originated there. And each day as the sun rises, the animal ones, the zooplankton, sink to the depths of the seas to avoid predators in such density that they appear on ship sonars like a new seabed, only to rise again at night in the largest migration of life on this planet.

With

Carol Robinson Professor of Marine Sciences at the University of East Anglia

Abigail McQuatters-Gollop Associate Professor of Marine Conservation at the University of Plymouth

And

Christopher Lowe Lecturer in Marine Biology at Swansea University

Producer: Simon Tillotson

Reading list:

Juli Berwald, Spineless: The Science of Jellyfish and the Art of Growing a Backbone (Riverhead Books, 2018)

Sir Alister Hardy, The Open Sea: The World of Plankton (first published 1959; Collins New Naturalist Library, 2009)

Richard Kirby, Ocean Drifters: A Secret World Beneath the Waves (Studio Cactus Ltd, 2010)

Robert Kunzig, Mapping the Deep: The Extraordinary Story of Ocean Science (Sort Of Books, 2000)

Christian Sardet, Plankton: Wonders of the Drifting World (University of Chicago Press, 2015)

Helen Scales, The Brilliant Abyss: True Tales of Exploring the Deep Sea, Discovering Hidden Life and Selling the Seabed (Bloomsbury Sigma, 2022)