Global warming from within ocean hydrothermal vents

Climate change is a comprehensive issue. Has the world always had climate changes? They were reported in the biblical book of Genesis of the Old Testament. Of course they didn’t track weather patterns then. Burning forests may be the result of human error – an incorrectly disposed cigarette. Hydrothermal vents deep in our seas and oceans are recent discoveries where molten magma meets nearly frozen water. Are warming waters a problem from these natural hydrothermal vents?

Climate change is one of the major challenges confronting the future of planet Earth as we know it. All those Deep Planet videos we might watch demonstrate that beneath the oceanic depths are cracks, fissures, nooks, crannies as dangerous as the highest mountains above sea levels. Discoveries of hydrothermal vents at the ocean bottoms raise serious questions of warming waters and melting ice. Are we cooking from within?

Seismologists track the planet surface movements 24/7 at hundreds of points. Their information is critical predicting earthquakes and earthquake severity. Some movements are like hums while others crackle and pop. Global warming from within occurs during those innocent hums. That’s when hydrothermal vents form.

Hydrothermal vents occur at both diverging and converging plate boundaries. Heat is released as magma rises and cracks the ocean floor and overlying sediments. Seawater drains into the fractures and becomes super-heated, dissolving minerals and concentrating sulfur and other compounds. Sea creatures in those depths either thrive or die. At those greater depths via exploration equipment technologies many thrive.

Cold water meshes with extremely hot molten rock magma as vents burst through ocean floor. Discovered only in 1977, hydrothermal vents are home to dozens of previously unknown species. Huge red-tipped tube worms, ghostly fish, strange shrimp with eyes on their backs and other unique species thrive in these extreme deep ocean ecosystems found near undersea volcanic chains. These are the fit that have survived the initial heat blasts of formed hydrothermal vents. For us, these vents are as foreign as radio waves from galaxies 900 million light years away. But they exist throughout our planet.

For the most part these occasional hydrothermal vents for magma are relatively small…a few centimeters. For the most part, earth crust at ocean temperatures act as potent barriers. Then there’s human impact. In the past, the main human impact affecting deep-sea ecosystems was the dumping or disposal of litter into the oceans. If it were only litter. Humans have tossed some heavy items and waste that landed on ocean floors. All it takes is a tiny crack and a century to make a hydrothermal vent.

Hydrothermal vents on the ocean floor may have some impact at releasing volcanic heat into our water systems, impacting ice formations and weather patterns as extreme heat converges with extreme cold. The severity is there may be communities of these hydrothermal vents deregulating a regulation system formed over millions of years.

People use hydrothermal energy for survival. Regulation of body temperature in vertebrates is a function of a central mechanism and the main thermoregulatory organ is again the hypothalamus, particularly the preoptic area (POA), where the sensory input on the brain temperature and core temperature is integrated. Other parts of the central nervous system, such as the brainstem and spinal cord, are also involved in thermo-regulation. Our bodies sweat because our skin has pores that help maintain thermoregulation.

Your hypothalamus is a section of your brain that controls thermoregulation. When it senses your internal temperature becoming too low or high, it sends signals to your muscles, organs, glands, and nervous system. They respond in a variety of ways to help return your temperature to normal.

The problems encountering ocean floor regularization are that if there may be one vent then there may be more hydrothermal vents forming a community. Each involves a hot/cold exchange and regulation is a war of average potentials.

And that process helps sustain a deep ocean balance. Most living things on earth depend on sunlight as the ultimate source of energy. Green plants use sunlight to make food by the process of photosynthesis. In the darkness of the ocean depths there is no sunlight for photosynthesis. So how do living things survive in such an environment? The answer is found in bacteria that can use another source of energy to make food.

Water coming out of a vent is rich not only in dissolved minerals but also in chemosynthetic bacteria. These bacteria are capable of utilizing sulfur compounds to produce organic material through the process of chemosynthesis. The bacteria are autotrophs that oxidize hydrogen sulfide in vent water to obtain energy, which is used to produce organic material (i.e. grow themselves).

Chemosynthetic bacteria are the primary producers and form the base of vent food webs. All vent animals ultimately depend on the bacteria for food. So hydrothermal vents are very beneficial to creatures living at the dark oceanic depths. For all we know, these vent/water exchanges have been present since the earth first developed its crust. Billions of years ago, according to science theoretical models.

Presence of hydrothermal vents probably have little to do with global warming. Releasing noxious gas and waste into our ecosystems may have had more impact. These vents may be natural players that rewrite regulation parameters of planetary climates. Climate change refers to the changes in the global climate which result from the increasing average global temperature. For example, changes in precipitation patterns, increased prevalence of droughts, heat waves, and other extreme weather, etc.

The debate is serious. On the nay side, earth’s weather patterns have only been recorded for the past 150 years. Yet, since the industrial revolution, about 300 years ago, new chemicals found their way into our vast ecosystem. Also, we are discovering more fluctuations of the space of our solar system and scientists are exploring phenomena such as hydrothermal vents. So there are statistical outliers that boggle finite conclusions. But, in our lifetimes, changes in climates have been observed.

Within hydrothermal vents, influences on water temperatures are vague. Hydrothermal fluid temperatures can reach 400°C (750°F) or more, but they do not boil under the extreme pressure of the deep ocean. As they pour out of a vent, the fluids encounter cold, oxygenated seawater, causing another, more rapid series of chemical reactions to occur.

Based on global water temperature statistics: The average temperature of the entire ocean surfaces usually ranges from 15 to 17 degrees Celsius (59 to 62.9 degrees Fahrenheit). There is a barrier between the surface water and deeper layers of the ocean that are not mixed. The barrier begins around 100 meters and can extend another few hundred meters downward. The average temperature of deep-ocean water is only 2°C (36°F). The water coming directly from a hydrothermal vent can reach up to 350°C (662°F) and is rich in dissolved chemicals. The hot spring water forms a plume above the vent, somewhat like smoke rising from a chimney into the air. Temperature-sensing instruments, towed behind research vessels, can detect these hot-water plumes and aid oceanographers in locating hydrothermal vents on the ocean floor.

Like hot springs and geysers on land, hydrothermal vents form in volcanically active areas—often on mid-ocean ridges, where Earth’s tectonic plates are spreading apart and where magma wells up to the surface or close beneath the seafloor.

These hot plumes of water from reactions with hydrothermal vents may contribute to ocean water temperatures from within.

As far as carbon dioxide releases into the air, results revealed that dissolved organic carbon is efficiently removed from ocean water when heated. The organic molecules are broken down and the carbon converted to carbon dioxide. The entire ocean volume circulates through hydrothermal vents about every 40 million years, according to theorists studying at University of Georgia.

Climate effects from vast forest fires, waste disposal, and gluttony for fossil fuels may be stressing our planetary biomes. They may arise from ignorance, irresponsibility, profit, convenience, and other factors. The vast fires of Australia may have been started by campers and smokers. 14 people have been arrested. Humans and humanity may be more significant drivers of climate changes than hydrothermal vents.

On seismology offices the earth is humming. Is it a happy or sad tune?

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