by simon
Why are the oceans important? The importance of wildlife.

The importance of the oceans, their wildlife and ecosystems

The land and oceans are part of one system: Earth. So when we ask, why are the oceans important? We’re asking about our own future. Life began in the ocean billions of years before the first plants or animals colonised land. Oceans regulate the state of our atmosphere because they are 99 per cent of the volume of living space for animals and wildlife is the mechanism that drives stability.

Climate change has always been the symptom of biodiversity loss … that’s to say, the breakdown of the complex connectivity between lifeforms that allows Earth to flex in response to changing conditions. Ocean wildlife has, for the large part, acted as a buffer against the most catastrophic effects and since about fifty million years ago, has kept our climate quite stable.

Industrial fishing only happened recently in our planet’s history and this reduction in the abundance of wildlife represents our greatest challenge for survival.

Below you will find a range of articles designed to inspire an understanding of the magnitude of animal impact on our oceans.

What’s more important, the ocean or the land?

The importance we bestow on the land is anthropocentric because we live there. It’s naturally important to us that we protect it. Nonetheless, if life in the ocean dies, we suffer irreversible changes to land-based ecosystems and climate.

In this article, we take a look at many of the ways that land and oceans are linked together.

The answer to the question, ‘why are the oceans important’, is that we live on the land but the oceans regulate Earth’s temperature. The oceans are equally vital to the land we live on.

Latest posts about why the oceans are important

Prehistoric Earth, Drawing by Simon Mustoe
How did life begin? A simple chronology of life for the last billion years!
What Earth probably looked like a billion years ago. There were no animals or plants. It was relatively warm and the skies were clear, except for erupting volcanoes. Cyanobacteria had started to invade the shallows, where they would deposit sediment in the form of mushroom-shaped Stromatolites. You can still see Stromatolites on the edge of the Indian Ocean at Hamelin Pool in Western Australia. Drawing by Simon Mustoe.

How did life begin?

I was inspired by a video posted online [1] that accompanies a new paper showing tectonic plate movement over the last billion years. It’s always interesting to ask ‘how did life begin?’ I thought it would be fun to look at the evolution of animal life as it’s often hard to comprehend. Evolution isn’t a steady continuum. Ever since the very first multicellular lifeforms appeared, it has been accelerating, and is punctuated by periods of immense disruption. It’s a reminder, that animals have been instrumental in controlling the disturbance caused by photosynthesising algae and plants. We owe a lot to animals. Without them, the plants would take over and we’d not have a habitable Earth.

History of life on Earth

A billion years ago

1,000 mya A soup of cyanobacteria develop natural sunscreen against the Sun’s blistering UV radiation. There’s scarcely any oxygen and no ozone layer yet. This enables them to reach the surface and start photosynthesising. They begin to saturate the ocean with oxygen. This leaks into the atmosphere and starts combining with methane (a powerful greenhouse gas).

750 mya Snowball Earth happens … stripped of methane, the planet is plunged into an ice-age that lasts 120 million years. This massively accelerates the rate of evolution. This means bacteria can form symbiotic relationships and become multicellular, then under the cold conditions, speciation develops fast.

650 mya The first bilaterally symmetrical animals (Ediacaran fauna) appear in the oceans. This heralds the dawn of a new age of marine animals that diversify to all shapes and sizes. Coral reefs colonies almost all the oceans.

Half a billion years ago

470 mya The first plants start to colonise land. They strip carbon dioxide from the atmosphere, weather rocks, create soil and pollute the ocean with these chemicals. This action starts to literally starve ocean life of oxygen.

375 mya The Devonian mass extinction happens. The waste from planet-eating plants manage to kill three-quarter of animal life, all of which is currently in the ocean. Ediacaran fauna is wiped from existence.

350 mya Animal life begins re-evolving into new forms and starts to colonise the land. Finally they get control of the planet-killing plants and beginning to stabilise the coupled ocean-atmosphere climate systems.

230 mya The first dinosaurs appear. The warm, oxygen-rich climate suits them so well, they spread out among the adjoined continents. Large animals dominate Earth’s ecosystems for another 165 million years .

A hundred million years ago

66 mya a damn meteor hits Earth killing most life on Earth and wiping out most dinosaurs for good . It takes another 10 million years or so before the planet’s wildlife starts to recover.

30 mya life reforms in its new design of hairy mammals and feathered dinosaurs (birds). It takes about 25 million years, for ecosystems to reach full capacity again.

10 mya animals have stabilised the climate. They have created present-day ecosystems, sufficiently diverse to support the evolution of even more complex life forms. The temperature of the Earth, the stability of climate and predictable abundance of food, enables the evolution of sophisticated primates. Orangutans, gorillas and chimpanzees evolve.

A million years ago

2 mya the first ancestors of modern humans evolved and began killing all the megafauna.

300,000 ya Earth finally becomes suitable for modern humans to be the next most likely species to evolve and survive.

The next chapter of life on Earth will be ours … the story is to be continued.

Reference (for the plate tectonic map):

  1. Merdith et al. (2021) Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic. Earth-Science Reviews, Volume 214, March 2021, 103477. https://www.sciencedirect.com/science/article/abs/pii/S0012825220305237
0 FacebookTwitterPinterestLinkedinRedditWhatsappEmail

This website uses cookies to improve your experience. We'll assume you're ok with this, but you can opt-out if you wish. Accept Read More