EXTREMOPHILES: SALINITY AND AT LOW NUTRIENT LEVELS

BY DAKSHITA NAITHANI

Prokaryotic life has dominated much of our planet’s evolutionary history, developing to fill nearly every possible environmental niche. Extremophiles are one of these. Extremophiles have been identified on Earth that can survive in conditions that were previously considered to be inhospitable to life. Heat, extremely acidic conditions, extreme pressure, and extreme cold are examples of extreme environments. The thermophiles were the first extremophiles to be discovered in the 1960s by Thomas Brock of Indiana University. He was investigating life in Yellowstone National Park’s super-hot water pools. He discovered tiny microorganism mats at Octopus Spring in 1965, when temperatures reached 175 degrees Fahrenheit. Thermus aquaticus was discovered, which led to the discovery of PCR and the creation of a new multibillion-dollar enterprise.

EXTREMOPHILES IN SALINITY: HALOPHILES

The halophiles live in high salt concentrations and are named after the Greek term for “salt-loving.” While the majority of halophiles belong to the archaea domain, some bacterial halophiles and eukaryotic species, such as the alga Dunaliella salina and the fungus Wallemia ichthyophaga, do not. Carotenoid chemicals give certain well-known species, such as bacteriorhodopsin, a red hue. They may be found in salty water bodies such as the Great Salt Lake in Utah, Owens Lake in California, the Dead Sea, and evaporation ponds, where the salt content is more than five times that of the ocean. They’re thought to be a viable contender for extremophiles living in Jupiter’s Europa and other comparable moons’ salty subsurface water oceans.

CELLULAR ADAPTATIONS BY HALOPHILES

High salt-in strategy

The high-salt-in approach protects halophiles from a saline environment by accumulating inorganic ions intracellularly and balancing the salt content in their surroundings through KCl influx. Cl- pumps, which are only found in halophiles and transfer them from the environment into the cytoplasm, are involved in this process. Extreme halophiles of the archaeal and bacterial families keep their osmotic equilibrium by concentrating K + inside their cells. The membrane-bound proton-pump bacteriorhodopsin works to accomplish this.

Low-salt, organic solute-in strategy

The high-salt-in approach necessitates physical modification of all macromolecules in order to survive in a very saline environment, which is incompatible with the survival of moderate halophiles that flourish in salinity-varying environments. Osmolytes protect microbial proteins against dissociation in low-salt water while also improving the bacteria’ tolerance to drastic changes in external saline conditions. Glycine betaine was the first bacterial osmolyte discovered in Halorhodospria halochloris.

The majority of halophiles are unable to thrive outside of their high-salt natural habitats. Many halophiles are so delicate that putting them in distilled water causes them to lyse due to the shift in osmotic circumstances. Halophiles include phototrophic, fermentative, sulfate-reducing, homoacetogenic, and methanogenic species in anaerobic conditions whereas in aerobic conditions include phototrophic, fermentative, sulfate-reducing, homoacetogenic, and methanogenic species.

The Haloarchaea, notably the Halobacteriaceae family, belong to the Archaea domain and make up the bulk of the population in hypersaline settings. The family currently has 15 recognised genera. Bacteria (mostly Salinibacter ruber) can make up to 25% of the prokaryotic community, although it usually makes up a considerably smaller portion of the overall population. In this habitat, the alga Dunaliella salina can sometimes thrive.

EXTREMOPHILES AT LOW NUTRIENT LEVELS: OLIGOTROPHS

An oligotroph is an organism that can survive in a low-nutrient environment. Oligotrophs are usually known for their sluggish development, low metabolic rates, and sparse population density. The settings are ones that provide little in the way of life support. Deep marine sediments, caverns, glacial and polar ice, deep underground soil, aquifers, and leached soils are examples of these habitats.

The cave-dwelling olm the bacteria Pelagibacter ubique, which is the most numerous creature in the seas and lichens with their incredibly low metabolism are all examples of oligotrophic species.

Caulobacter crescentus is an oligotrophic Gram-negative bacteria found in freshwater waterbodies. The whole cell functions as an integrated system in the control circuitry that controls and paces Caulobacter cell cycle development. As it orchestrates activation of cell cycle subsystems and Caulobacter crescentus asymmetric cell division, the control circuitry monitors the environment and the internal status of the cell, including the cell topology. The control system has been meticulously tuned as a whole system for reliable functioning in the face of internal stochastic noise and external unpredictability by evolutionary selection.

The bacterial cell’s control system is organised in a hierarchical manner. The signalling and control subsystem communicates with the outside world through sensory units that are mostly found on the cell surface. To adjust the cell to current conditions, the genetic network logic responds to signals received from the environment as well as internal cell status sensors.

ENVIRONMENT AND LOCATIONS

Oligotrophic lakes are often found in northern Minnesota, with deep clear water, stony or sandy bottoms, and minimal algae.

Oxygen levels are high throughout the water column in oligotrophic lakes. Cold water may store more dissolved oxygen than warm water, thus oligotrophic lakes’ deep regions remain quite cold. Low algal content also provides for more light penetration and less breakdown. Algae, zooplankton, and fish die and are degraded by bacteria and invertebrates at the bottom of the ocean. The process of breakdown consumes oxygen. 

Locations

 Oligotrophs and eutrophs coexist in natural ecosystems, and their proportions are determined by an individual’s capacity to prevail in a given environment.  Despite their capacity to exist in low-nutrient settings, they may struggle to survive in nutritionally- rich ones. Most microorganisms are not well adapted to exist in nutrient-limited circumstances and frigid temperatures (below 5 °C), Antarctic habitats offer very little to sustain life. Some of the documented examples of oligotrophic environments in Antarctica are:

Lake Vostok, a freshwater lake cut off from the rest of the world by 4 kilometres (2.5 miles) of Antarctic ice, is often cited as a prime example of an oligotrophic ecosystem. Because of the lake’s severe oligotrophy, some people assume that sections of it are entirely sterile. This may be used as a model to simulate alien life investigations on frozen planets and other celestial worlds.

Oligotrophic soil environments

In general, nutrient availability decreases as the depth of the soil environment increases, since organic molecules degraded from detritus are swiftly eaten by other microorganisms on the surface, resulting in nutritional deficiency in the deeper levels of soil.

Collimonas is one of those species that may survive in an oligotrophic environment as it has the capacity to not only hydrolyze the chitin generated by fungus for nutrition, but also to create materials. Fungi are a prevalent element of the habitats where Collimonas thrives. In oligotrophic settings, reciprocal relationships are prevalent. Weathering also allows Collimonas to access electron sources from rocks and minerals.

The environment of soil in polar locations, such as the Antarctic and Arctic regions, is termed oligotrophic since the soil is frozen and biological activity is minimal. Actinobacteria, Proteobacteria, and Cyanobacteria are the most common bacteria in frozen soil, with a tiny quantity of archaea and fungus. Under a wide range of low temperatures, actinobacteria can keep their metabolic enzymes active and continue their biochemical processes.

The following are the characteristics that a bacterium should have in order to be labelled as an oligotroph:

(a) Having a form with a high surface-to-volume ratio.

(b) Having an innate propensity for using metabolic energy for food absorption during phases of growth stagnation.

(c) Possessing nutrition absorption abilities that are expressed in a constitutive manner.

(d) Presence of a low-specificity, high-affinity transport mechanism that allows for simultaneous absorption of mixed substrate.

 (e) Having systems for conserving nutrition after it has been absorbed.

Extremophiles and their products have revolutionised many aspects of our home and professional life, from household materials to molecular diagnostics. It is not unlikely that new and medically useful discoveries will be found in the realm of extremophile research; the potential of these organisms is so fresh and huge that their applications may be restricted only by imaginations.

An massive iceberg, approx. the size of New Delhi broke off in Antarctica

(Image credit: Halley team/British Antarctic Survey)

An iceberg of 1270 sq. km in size has broken off from Antarctica. This happened in the Burnt Ice Shelf, the Iceberg is apparently is of the shape of Indian capital New Delhi. According to the reports it was breaking at the rate of 1km per day.

Icebergs are pieces of ice that have broken off from glaciers or ice shelves and are now floating in open water, according to the National Oceanic and Atmospheric Administration.

The North Rift crack grew toward the northeast at a rate of about 0.6 miles (1 km) per day in January; but on the morning of Feb. 26, the crack widened a couple hundred meters in just hours. This ice split happened due to a natural process, and there’s no evidence that climate change played a role, according to the statement. The Brunt Ice Shelf, a 492-foot-thick (150 meters) slab of ice, flows west at 1.2 miles (2 km) per year and routinely calves icebergs.

The thickness of the iceberg is 150 meters. A picture of this has also been released by the British Antarctic Survey. According to scientists the incident occurred in the Burnt Ice Shelf area. This disintegration is called ‘calving’, in which vast icebergs separate from the frozen area.

The current calving was first recorded in November 2020. By January 2021, the speed of its breakdown had reached one km per day, on Friday it was eventually declared broken. There is so much snow on Antarctica that if it breaks and melts in the sea, the water level will rise by 70 meters. Many cities and islands will be completely submerged.

Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. It is a form of ice ablation or ice disruption. It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf.

According to researchers “Our teams at B.A.S.(British Antarctic Survey) have been prepared for the calving of an iceberg from Brunt Ice Shelf for years,” Dame Jane Francis, the director of the B.A.S., said in a statement. “Over coming weeks or months, the iceberg may move away; or it could run aground and remain close to Brunt Ice Shelf.”

Why do icebergs melt?

When an iceberg reaches warm waters, the new climate attacks it from all sides. On the iceberg surface, warm air melts snow and ice into pools called melt ponds that can trickle through the iceberg and widen cracks. At the same time, warm water laps at the iceberg edges, melting the ice and causing chunks of ice to break off. On the underside, warmer waters melt the iceberg from the bottom up. This phenomenon of ice-calving happens over a long period of time but the fast paced climate change had accelerated the process.

Loss Of Ice Cover In The Arctic Sea

The National Centre of Polar and Ocean Research (NCPOR) recently found the largest decline in the Arctic Sea ice as seen in last 41 years due to global warming in July 2019.

Between 1979 and 2018, NCPOR noted that the sea ice has seen a declination at a rate of -4.7 per cent per decade while its rate in July 2019 was found to be -13 per cent.

Sea ice is basically frozen seawater that floats on the ocean surface. It forms in each hemisphere’s winter of both the Arctic and the Antarctic. The ice retreats in the summer. However, it does not completely disappear.

The Research has clarified that if this trend continues, there would be no ice left by 2050 in the Arctic sea since the volume of ice loss during summers might surpass the volume of the same formed during winters. This rapid decline in Arctic sea ice cover has been linked with growing carbon emissions and subsequent global warming.

The Impacts of Declining Arctic Sea ice cover can be huge. It would have an influence on regional weather as the decline of sea ice may impact the evaporation rates, cloud cover, air humility and rainfall of neighbouring regions.

The National Centre for Polar and Ocean Research (NCPOR) was established in 1998 as an autonomous Research and Development Institution under the Ministry of Earth Sciences. The objective was to primarily carry out research activities in the polar and Southern Ocean realms.

It is also responsible for maintenance of the Indian stations in Arctic (Himadri) and Antarctica (Maitri & Bharati).

In recent times, the high temperatures that have been recorded in the Siberian region have caused a prolonged heatwave that has been ascribed to the absence of sea ice among other factors.

Loss of habitat for seals and polar bears have also increased resulting encounters between polar bears and humans. As the sea ice retreats from coastlines, wind-driven waves combined with melting permafrost may also lead to more rapid coastal erosion.

In the Arctic region, the ocean circulation is driven by the sinking of dense and salty water. Fresh meltwater coming largely from the Greenland Ice Sheet could furthermore interfere with ocean circulation at high latitudes, ultimately slowing it down. Any changes in ocean circulations can have unpredictable global impacts even in lower latitudes such as extreme weather events, droughts etc.

It is a result from the positive feedback cycle known as the ice-albedo feedback states that sea ice has higher albedo than ocean water. Once sea ice begins to melt, a self-reinforcing cycle often begins whereby as more ice melts and exposes more dark water. Then the water absorbs more sunlight and the sun-warm water then melts more ice.

On concluding, Arctic sea ice is part of a complex global system, and as a result it affects communities at all latitudes. The loss of Arctic sea ice has to be slowed down existentially by reducing carbon dioxide and other greenhouse gas emissions and also by conserving other natural resources that have global impacts. The world needs to come together as one.