The Singing Frogs of Northeast India: Nature's Hidden Melodists

Photographer: Alen Alex

Debolina Banerjee

Northeast India is home to some of the world's most unique and rare species because it has so many different kinds of plants and animals. The Singing Frogs are one of the most interesting and least-studied of all the wonders. They are a group of amphibians known for their melodic voices and complex ways of communicating. These frogs sing in different rhythms than their more common relatives. Some even make sounds that sound like bird song or insect chirps. All other frogs croak.

A Symphony in the Rain

Indeed, it is in the dense forests and hilly landscapes of the Northeast that these musical frogs find their ideal haven. In the forests of Arunachal Pradesh, Assam, and Meghalaya, there are many types of music frogs. Some of them are new to science, like the rare Jerdon's Tree Frog (Hyla annectans) and the Bamboo Tree Frog (Chirixalus doriae).

During the monsoon, they make a magical symphony that echoes through the forest, like an orchestra made of living things. Male frogs use their calls to mark their territory, attract females, and even warn other frogs about possible dangers. In a loud mix of sounds, each species uses its own call to find other members of its own species.

The Exceptional Case of the Assam Painted Frog

The Assam Painted Frog (Uperodon taprobanicus) is one of the most unusual amphibians in the area because of its bright colours and strange mating calls. This frog makes a common mating call by whistling like a flute instead of making the low throat noises that most other frogs do. The calls are said to sound like insects to scare off predators without giving away their location, which leaves the door open for potential mates.

The Assam Painted Frog lays its eggs in tree hollows or leaf litter pools that are hard to find, while many other frogs lay their eggs in open water. This change makes it more likely that the tadpoles will live and less likely that they will be eaten, which is a very important strategy in forests with a lot of predators.

Unusual Communication: Clicking, Trilling, and Whistling

What sets them apart is the variety in the call structure of these frogs. Most amphibians use simple croaks, while these singing frogs of Northeast India came up with unique vocal strategies:

• Clicking Calls: In some species, such as the Bamboo Tree Frog, crisp clicking sounds, almost like snapping fingers, are emitted. Very frequently these are used consecutively to signal dominance.

•Trilling Songs: Frogs, like the Jerdon's Tree Frog, are known to utter trilling long notes, much like a cricket. These kinds of sounds travel further through thick forests and serve their purpose in communication.

•Whistle-like Tunes: Frogs, like the Assam Painted Frog, are known to produce melodious whistles. This may be an evolutionary trait for communication so as not to invite snakes or even birds.

The Challenges of Conservation

Even with such interesting adaptations, these special frogs are confronted with serious threats. Very few of these are currently threatened due to habitat loss caused by deforestation, agriculture, and lately, by climate change. Further, pollution and an increasing proliferation of fungal diseases such as chytridiomycosis, which has already caused widespread death in frog species throughout the world, may threaten many of these species.

Conservationists are trying to document and preserve these threatened amphibians before they actually disappear. Community education, wetland conservation, and habitat conservation programs are being initiated throughout the region. Scientists say that long-term observation of these species will be necessary to understand their ecological functions and ensure their survival.

A Hidden Treasure of Nature

The singing frogs of northeastern India remind us of nature's wonders. Complex calls, intriguing habits, and intriguing adaptations further highlight the complexity of life in one of the most biodiverse parts of the world. Save these natural songsters, primarily to maintain the delicate balance of ecosystems that depend on frogs.

The next time any of us find ourselves in the rainforests of Meghalaya, Assam, or Arunachal Pradesh, let's stop and listen. Their song is a nature reminder of a beauty that persists and deserves to be sought out and protected.

The writer is a zealous environmentalist and emerging conservationist with six years of experience working in the fields of Environmental Science, Wildlife Conservation, and Sustainable Management. Committed to promoting balance between individuals and the environment through evidentiary research, fieldwork, and activism.

Photographer: Alen Alex 

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What’s a ‘Strombolian eruption’? A volcanologist explains what happened at Mount Etna

Thermal camera images show the eruption and flows of lava down the side of Mount Etna. National Institute of Geophysics and Volcanology, CC BY

Teresa Ubide, The University of Queensland

On Monday morning local time, a huge cloud of ash, hot gas and rock fragments began spewing from Italy’s Mount Etna.

An enormous plume was seen stretching several kilometres into the sky from the mountain on the island of Sicily, which is the largest active volcano in Europe.

While the blast created an impressive sight, the eruption resulted in no reported injuries or damage and barely even disrupted flights on or off the island. Mount Etna eruptions are commonly described as “Strombolian eruptions” – though as we will see, that may not apply to this event.

What happened at Etna?

The eruption began with an increase of pressure in the hot gases inside the volcano. This led to the partial collapse of part of one of the craters atop Etna.

The collapse allowed what is called a pyroclastic flow: a fast-moving cloud of ash, hot gas and fragments of rock bursting out from inside the volcano.

Thermal camera images show the eruption and flows of lava down the side of Mount Etna. National Institute of Geophysics and Volcanology, CC BY

Next, lava began to flow in three different directions down the mountainside. These flows are now cooling down. On Monday evening, Italy’s National Institute of Geophysics and Volcanology announced the volcanic activity had ended.

Etna is one of the most active volcanoes in the world, so this eruption is reasonably normal.

What is a Strombolian eruption?

Volcanologists classify eruptions by how explosive they are. More explosive eruptions tend to be more dangerous, because they move faster and cover a larger area.

At the mildest end are Hawaiian eruptions. You have probably seen pictures of these: lava flowing sedately down the slope of the volcano. The lava damages whatever it runs into, but it’s a relatively local effect.

As eruptions grow more explosive, they send ash and rock fragments flying further afield.

At the more explosive end of the scale are Plinian eruptions. These include the famous eruption of Mount Vesuvius in 79AD, described by the Roman writer Pliny the Younger, which buried the Roman towns of Pompeii and Herculaneum under metres of ash.

In a Plinian eruption, hot gas, ash, and rock can explode high enough to reach the stratosphere – and when the eruption column collapses, the debris falls to Earth and can wreak terrifying destruction over a huge area.

What about Strombolian eruptions? These relatively mild eruptions are named after Stromboli, another Italian volcano which belches out a minor eruption every 10 to 20 minutes.

In a Strombolian eruption, chunks of rock and cinders may travel tens or hundreds of metres through the air, but rarely further. The pyroclastic flow from yesterday’s eruption at Etna was rather more explosive than this – so it wasn’t strictly Strombolian.

Can we forecast volcano eruptions?

Volcanic eruptions are a bit like weather. They are very hard to predict in detail, but we are a lot better than we used to be at forecasting them.

To understand what a volcano will do in the future, we first need to know what is happening inside it right now. We can’t look inside directly, but we do have indirect measurements.

For example, before an eruption magma travels from deep inside the Earth up to the surface. On the way, it pushes rocks apart and can generate earthquakes. If we record the vibrations of these quakes, we can track the magma’s journey from the depths.

Rising magma can also make the ground near a volcano bulge upwards very slightly, by a few millimetres or centimetres. We can monitor this bulging, for example with satellites, to gather clues about an upcoming eruption.

Some volcanoes release gas even when they are not strictly erupting. We can measure the chemicals in this gas – and if they change, it can tell us that new magma is on its way to the surface.

When we have this information about what’s happening inside the volcano, we also need to understand its “personality” to know what the information means for future eruptions.

Are volcanic eruptions more common than in the past?

As a volcanologist, I often hear from people that it seems there are more volcanic eruptions now than in the past. This is not the case.

What is happening, I tell them, is that we have better monitoring systems now, and a very active global media system. So we know about more eruptions – and even see photos of them.

Monitoring is extremely important. We are fortunate that many volcanoes in places such as Italy, the United States, Indonesia and New Zealand have excellent monitoring in place.

This monitoring allows local authorities to issue warnings when an eruption is imminent. For a visitor or tourist out to see the spectacular natural wonder of a volcano, listening to these warnings is all-important.The Conversation

Teresa Ubide, ARC Future Fellow and Associate Professor in Igneous Petrology/Volcanology, The University of Queensland

This article is republished from The Conversation under a Creative Commons license. Read the original article.

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