Saturday, October 04, 2025

 

Moscow Reaches Out To Buddhists Abroad But Faces Problems With Them At Home – Analysis

A Buryat boy in a shaman ritual in Siberia, Russia. Photo Credit: Аркадий Зарубин, Wikimedia Commons.


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Of Russia’s four traditional faiths, Buddhism, the third largest, garners far less attention than any of the others. This gives Moscow a greater opportunity to sell its version of Buddhist life in the Russian Federation without being challenged, as it does with Russian Orthodoxy, Islam, and Judaism. Unsurprisingly, the Kremlin has long exploited this situation to influence Buddhist countries.


As its influence elsewhere has slipped since Russian President Vladimir Putin began his expanded war against Ukraine, Moscow has stepped up its efforts to shore up or win additional support among Buddhist countries abroad. Just how far the Kremlin is prepared to go was signaled last week when it attracted more than 7,000 Buddhists from across the world to the Third International Buddhist Forum that Moscow organized in Kalmykia and to which Putin sent an effusively warm message (Asia Russia, September 27; III Mezhdunarodniy Buddiyskiy Forum, September 28).

Moscow media coverage of the event, unsurprisingly, was uniformly upbeat. This did little to conceal the growing anger and divisions within the Buddhist community in Russia, however, which have now become so intense that some Buddhists there describe their faith as having become “a protest religion” (Ekho, January 29, 2023). Nor could it obscure the ways Moscow has been forced to tailor its policies toward Buddhists within the country to cope with Kremlin concerns about the reactions of Mongolia which supports Buddhist dissidents from Russia, and of the Peoples Republic of China (PRC), which, because it is concerned about Buddhism in Tibet, favors a more repressive line (Window on Eurasia, February 5, 2023, August 8; see China Brief, September 19).

As a result, and despite the Moscow headlines, the latest forum has only complicated the Kremlin’s relations with the Buddhists both inside the Russian Federation and abroad, with some of the former now pursuing independence from Moscow and some of the latter increasingly alienated by it (Readovka, September 26).                          

The Buddhists of the Russian Federation number approximately 1.5 million, far fewer than the Russian Orthodox or the Muslims, but more than the Jews. Most of them live in Kalmykia in the North Caucasus or in Buryatia and Tyva, east of the Urals along the Mongolian border. In the 1920s and 1930s, the Soviet government banned Buddhism in the Soviet Union, making it the only major religion to be treated in this manner. When Stalin restored the Russian Orthodox Church leadership during World War II, however, he also sought to revive the Buddhist communities. Between the end of that war and until very recently, the center of Russian Buddhism was in Buryatia (Lyudi Baikala, February 14, 2023).

Problems with the longtime head of that faith in that region, Moscow’s fears that Ulaanbaatar was exploiting Buddhism to promote pan-Mongolism at Russia’s expense, and concerns about the PRC reaction to the Buddhist leadership given Buryatia’s ties with the Dalai Lama and Tibetan Buddhism, however, led to a change (Window on Eurasia, February 10, 2024).


After forcing out the Buddhist leader of Kalmykia, who was also too close to the Buddhists of Tibet, Moscow allowed the renewed Buryatia Buddhist leadership to open an office in Moscow and challenge the Buryat Buddhists for dominance of that faith in Russia (Window on Eurasia, August 8, 2024).

The Kremlin also sought to regain control of the Buddhist community in Tyva, which had become increasingly independent-minded and where Buddhism appears to have played a huge role in helping to maintain and strengthen national identity (Window on Eurasia, June 4, 2021).

These problems had been intensifying since the 1990s, largely because Buddhism had played the role of a national religion in the three republics where it was dominant. They became much more serious, however, after Putin launched his expanded invasion of Ukraine in 2022 (The Moscow Times, January 13; Meduza, August 6).

Buryats, Kalmyks, and Tyvans were just as divided about the war as other nations in the Russian Federation. Their religious leaders were even more so than most, despite the reputation Buryats who did join the Russian army have acquired in the Russian and Western media for being especially savage fighters (Window on Eurasia, February 16, 2023; January 19).

Many Buddhists—the exact number is unknown but likely totals several thousand or more—opposed to the war in all three republics fled to Mongolia, where they were welcomed (Window on Eurasia, October 28, 2022, February 3, 2024, August 8). At the same time, Moscow’s increasing reliance on the PRC made it ever more sensitive to and prepared to address Beijing’s concerns about contacts between Buddhists in the Russian Federation and those in Tibet, as well as Tibetan emigration (Readovka, September 26).

While speakers avoided these topics in their official presentations, it is certain that the representatives of Buddhists from more than 35 countries there could see what is animating the three Buddhist nations in the Russian Federation and how Moscow is trying to rein them in (III Mezhdunarodniy Buddiyskiy Forum, accessed October 2).

Moscow is employing its traditional divide-and-rule strategy by holding the meeting in Kalmykia, rather than the traditional center of Buryatia, and by announcing plans to open a Russian Buddhist University not in either of those regions, but in Tyva. These delegates also certainly heard an earful from some Buddhists of the Russian Federation on the sidelines, and the visitors could see by who was not present—anyone from the Tibetan Buddhist community of the Dalai Lama—how Moscow was seeking to meet Beijing’s demands.

The world’s Buddhists appear to be aware that the three Buddhist republics in Russia are radicalizing rapidly. In Buryatia, for example, there have been a series of demonstrations against Putin’s war against Ukraine and even calls for carrying passports to prove citizenship so that Russian nationalists will not attack Buryats (Astra Press, June 14; seePromethean Liberation, July 29).

In Kalmykia, some anti-war activists have even joined a unit that has gone to Ukraine to fight the Russian invaders, and a survey there has found that even the security forces in Kalmykia would actively support a post-Soviet and anti-Russian regime (Kavkaz Realii, August 24, 2023; Vot Tak, February 1).

In Tyva, official statistics now show that the republic has become the place where residents and visitors are the most likely to suffer as a result of violence (Esli Bit Tochnim, August 18, 2023). To add insult to injury, Moscow has declared the national movements of all three terrorist organizations (Mediazona; Govorit Nemoskva, January 11).  

Even taken together, this does not mean that the three Buddhist republics are about to declare independence, despite the hopes and even the predictions of some activists (Window on Eurasia, June 25, 2023). They are very small, isolated from one another, and landlocked. If the nationalist movements in them continue to grow and Moscow is forced to impose an even more repressive regime, however, the three will become even more radical, something that will be obvious to the world’s Buddhist community.

Moscow’s increasing deference to the PRC in its treatment of Buddhist faithful will also be visible. Those factors combined will make it unlikely that the Kremlin will gain the influence it seeks among Buddhists abroad, however many conferences, such as the one in Elista, it convenes.


Paul Goble

Paul Goble is a longtime specialist on ethnic and religious questions in Eurasia. Most recently, he was director of research and publications at the Azerbaijan Diplomatic Academy. Earlier, he served as vice dean for the social sciences and humanities at Audentes University in Tallinn and a senior research associate at the EuroCollege of the University of Tartu in Estonia. He has served in various capacities in the U.S. State Department, the Central Intelligence Agency and the International Broadcasting Bureau as well as at the Voice of America and Radio Free Europe/Radio Liberty and at the Carnegie Endowment for International Peace. Mr. Goble maintains the Window on Eurasia blog and can be contacted directly at paul.goble@gmail.com .

 

Can folds in rock layers strengthen the Earth's crust?




Tohoku University
Figure 1 

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(Left) Schematic illustration of a kink structure. (Center) Kink bands observed in mudstone near Fort Island, Rhode Island. (Right) Large-scale kink structure in Southern California, USA. 

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Credit: The right panel is modified from Davis and Namson (1994), Nature, the rest is ©Hiroaki Yokoyama et al.






Your first thought when describing a rock formation likely isn't a mille-feuille, but there are actually certain types composed of many thin layers that bring the flaky pastry to mind. Not only that - but these rocks can quite literally fold under pressure. These formations have the interesting ability to fold under compressive forces and form sharply localized bends known as kink bands. For many years, these kink bands were believed to reduce the mechanical strength of crustal rocks, weakening the Earth's outer shell.

However, a research group led by Professor Hiroyuki Nagahama, Professor Jun Muto, and Ph.D. Candidate Hiroaki Yokoyama at the Department of Earth Science, Tohoku University, has provided new experimental evidence that challenges this assumption. Their findings may improve our predictions of earthquake risk assessment to help protect communities in seismic zones.

Using biotite, a common mineral found in the Earth's crust that peels easily like a stack of paper due to its layered structure, the researchers conducted deformation experiments under varying pressure conditions. They found that when kink bands satisfy a specific geometric condition known as a rank-1 connection, the material exhibits strengthening rather than weakening. The rank-1 connection ensures smooth continuity between two differently deformed regions within the rock.

The group observed that kink bands with symmetric tilt boundaries led to a consistent increase in material strength. This phenomenon, known as kink strengthening, has been proposed in the field of materials science, but this study is among the first to clearly demonstrate it in natural geological materials.

"This study not only bridges concepts between materials science and geology, but also offers new insight into the mechanical behavior of the Earth's crust," says Nagahama.

To further strengthen the evidence of their findings outside of a controlled laboratory setting, the researchers also identified kink bands with similar geometric characteristics in real-world rock formations. These range from microscopic features within minerals to large-scale folds spanning kilometers, often referred to as mega kinks. The results suggest that such structures may locally enhance the strength of the crust and influence the distribution or location of earthquake ruptures.

"This finding may contribute to more accurate seismic hazard assessments in the future," says Yokoyama. "The more we understand about these rock formations, the better our predictions about earthquakes become. As such, this research could have a real positive effect on people living in earthquake-prone regions."

The findings were published in Scientific Reports on September 26, 2025.

Volcanic ash may enhance phytoplankton growth in the ocean over 100 km away



Nagoya University
Nishinoshima Island in the Ogasawara Islands of Japan 

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Nishinoshima Island, located in the Ogasawara Islands of Japan, is home to an active volcano. Ash from volcanic eruptions there in 2020 could have led to a temporary surge in phytoplankton levels in the seawater 130 km away.

 

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Credit: Ogasawara Village Tourism Bureau





A research group in Japan has suggested that ash released from volcanic eruptions on Nishinoshima Island—part of Japan's Ogasawara Islands—led to a temporary surge in phytoplankton levels in the seawater around Mukojima Island, which is located 130 km northeast of Nishinoshima and is also part of the Ogasawara Islands.

Mukojima lies within the subtropical gyre, a region known for low nutrient and low chlorophyll conditions. The study indicates that ash from the Nishinoshima eruptions was transported by wind and ocean currents to the waters around Mukojima, serving as a nutrient source for phytoplankton growth in that area.

The findings suggest that volcanic ash can enhance the productivity of marine waters even at considerable distances from the volcanic site. This study was published in the journal Progress in Earth and Planetary Science.

A large-scale volcanic eruption occurred at Nishinoshima between December 2019 and July 2020, releasing a substantial amount of ash into the ocean. Previous studies have shown higher levels of phytoplankton near the volcanic site. However, the effects of this ash on more distant areas were not well understood.

A group of researchers from Nagoya University, Tohoku University, Meiji University, and Waseda University, led by Professor Joji Ishizaka from the Institute for Space-Earth Environmental Research at Nagoya University, conducted a study to investigate the distant effects of ash from the Nishinoshima eruption.

The researchers analyzed satellite images of chlorophyll-a (Chl-a) around the Ogasawara Islands during the eruption of Nishinoshima. Generally, higher levels of Chl-a indicate a greater abundance of phytoplankton.

This study used two types of satellite image data. The first dataset was obtained from the Moderate Resolution Imaging Spectroradiometer sensor (MODIS) on NASA's Aqua satellite. Results showed that among the Ogasawara islands, Mukojima especially experienced a significant increase in Chl-a concentrations, rising from around 0.1 mg/m3 during the non-eruption period to a peak of nearly 0.2 mg/m3 during the eruption.

The second dataset was generated using data from the Japanese meteorological satellite Himawari-8, which was provided through the P-Tree System by JAXA. This dataset also confirmed an increase in Chl-a concentrations around Mukojima during the eruption period.

Based on these findings, the researchers hypothesized that the eruptions on Nishinoshima caused the increase in Chl-a around Mukojima. To verify this theory, they conducted numerical simulations using sea surface water velocity data from the Global Ocean Forecast System 3.1. They traced the movement of seawater with high Chl-a levels that reached the Mukojima area after transport of the ash by wind.

The results supported the hypothesis, demonstrating that the increase in Chl-a observed near Mukojima on July 4 was due to the volcanic ash released on Nishinoshima on June 28, six days prior.

Professor Ishizaka stated, "Our analyses of satellite data and numerical simulations suggest that the eruptions on Nishinoshima likely caused a phytoplankton bloom near Mukojima."

He explained, "Volcanic ash from the eruptions was released into the atmosphere and fell along the smoke to the northeast. The ash-containing seawater then traveled approximately 130 km to Mukojima. During this journey, the ash acted as a nutrient, promoting the growth of phytoplankton. Consequently, we observed a significant increase in phytoplankton around Mukojima six days later."

This study demonstrated that nutrients from volcanic eruptions can boost phytoplankton growth in areas with limited nutrients, even those far from the eruption site. These findings improve our understanding of ocean ecosystem dynamics and lay the groundwork for further research on the complex effects of volcanic activity on local ecosystems.

About the research team
This research was conducted over the course of more than two years by a team of students from Nagoya University, Tohoku University, Meiji University, and Waseda University, under the leadership of Professor Ishizaka. The students had formerly participated in the Advanced Satellite Training Course, which was organized by the Center for Orbital and Suborbital Observation at Nagoya University's Institute for Space-Earth Environmental Research.

 
 

Volcanic plume on June 28, 2020 (Left) and high chlorophyll-a area (Right) by Himawari-8. Red arrow in the right indicates the volcanic plume on June 28, 2020. Yellow arrow in the right indicates movement of water detected by the model.


 

Credit

Joji Ishizaka