Oceans For Dummies. Joseph Kraynak

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      Life in the low intertidal region is more aquatic; no surprise there, because everything’s submerged most of the day. Here, you find soft-bodied organisms, such as sea stars, sea slugs, sea urchins, and sponges, maybe even the occasional octopus (Philippe’s favorite sea creature), as well as turfing algae and seaweeds (marine plants that form mats).

      Remember Algae is a staple of intertidal communities, forming the basis of most food webs.

      Funfact White COOL AND CREEPY

      You wouldn’t know it from looking at them, but sea stars are vicious predators — carnivores that can muscle open mussels and clams using their five mighty suction-cup-equipped arms. But that’s not even the coolest part. After gaining entrance, they literally spill their guts, ejecting their stomachs from inside their bodies, through their mouths to digest their prey. After dining, they suck their stomachs back in (not just in a vain attempt to look more fit). And they wonder why they can’t get anyone to come over for dinner.

      Wading through the neritic zone

      When you start to need some sort of flotation device (or a boat) to keep your head above water, you’re in the neritic zone (also known as the sublittoral zone). This area starts at the low tide mark and continues to the edge of the continental shelf in the ocean — about 200 meters (660 feet) deep. While that may sound really deep, it’s relatively shallow compared to how deep it gets out in the open ocean, which is much, much, much deeper.

      Biodiversity is at its peak in the neritic zone, and no wonder — everyone wants to live here! Virtually every marine plant and thousands of coastal animal species (vertebrates and invertebrates) call this zone home. Consequently, the neritic zone is where 90 percent of all marine life resides. Diverse ecosystems flourish in and around coral reefs, seagrass beds, and kelp forests, all of which rely on sunlight-powered photosynthesis.

      Why is it such a popular place? Well, conditions in the neritic zone are ideal for supporting diverse marine communities — the presence of sunlight throughout the zone; moderate, stable temperatures, pressures, and salinity; plenty of oxygen and carbon dioxide; and an abundance of nutrients that make their way from the land into the ocean (which under normal circumstances is good but can be bad when it’s too much).

      funfact Even though the neritic zone accounts for only about 10 percent of the ocean, it produces roughly 90 percent of all the fish and shellfish we harvest, making it very valuable for us humans too.

      Heading out to sea: The oceanic zone

      The rest of the ocean that is neither intertidal nor neritic accounts for the oceanic zone. This vast, deep, inground pool comprises a huge chunk of Earth. It actually accounts for 95 percent of all the living space on the planet. Yet, it’s the part of the ocean (and part of the planet) we know the least about.

      It starts from the edge of the continental shelf (the outer edge of the neritic zone) and extends all the way down to the seafloor 11,064 meters (36,300 feet) at its deepest point at the bottom of the Mariana (or Marians) Trench. In fact, it’s so deep, it had to be divided into zones, but let’s not get too deep into that here; depth is the topic of the next section.

      While the diversity of species in the oceanic zone can’t hold a candle to the diversity in the neritic zone, the contrast in how life survives at the top and bottom of this zone can’t be beat. Near the surface, where sunlight penetrates, plants anchor the food webs and ecosystems. In contrast, on the seafloor, where it’s pitch black, ecosystems depend on either the remains of organisms that settle to the bottom or life that develops around hydrothermal vents and the bacteria that dine on the chemicals spewing from those vents.

      So, what sort of life exists in the oceanic zone? Keep reading.

      Funfact White HOW IS THE OCEAN LIKE A DESERT?

Schematic illustration of the ocean’s vertical zones.

      ©John Wiley & Sons, Inc.

      FIGURE 4-2: The ocean’s vertical zones.

      Skimming the surface: The epipelagic zone

      The epipelagic zone (commonly referred to as the sunlight zone) is the top 200 meters (about 650 feet) of the ocean, where enough sunlight is available for plant life to grow and support a large, diverse population of marine life. Because it forms the ocean’s surface, the epipelagic zone experiences greater variations (compared to the other vertical zones) in temperature and other conditions due to climate, local weather patterns, and proximity to large land masses.

Photo depicts Plankton.

      Courtesy of Christian Sardet/CNRS/Tara expeditions, from Plankton—Wonders of the Drifting World, Univ Chicago Press 2015. Licensed under CC BY-SA 4.0

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