Ecological Assessment of Lake Baikal near the Settlement of Bol’shye Koty

 

Participants

Elena Lavrentieva (Russia—Buryat Republic)

Marilyn Phelps (U.S.A.—Minnesota)

Oksana Pugach (Russia—Irkutsk)

Tatiana Serykh (Russia—Moscow)

Maxim Shapirov (Russia—Buryat Republic)

 

Leaders

            Maxim Timofeyev

            Zhanna Shatilina

            Kuzma Kirichenko

 

Overview

Lake Baikal in eastern Siberia, Russia, has six characteristics that combined make it a very unique and worthwhile subject of study.  Baikal has (1) a wide diversity of species; (2) a high level of endemism among its species; (3) a lack of mixing of its species with the species surrounding it in Eastern Siberia; (4) development of fauna in the lake’s deep depressions; (5) the presence of giant and dwarf forms of the same organisms; and (6) the relatively rapid evolution within the lake.  There are 2500 species of animals and 1500 species of plants found in Lake Baikal.  Of the fauna, 85% of the species are endemic, while 40% of the floral species are endemic.  Further, the lake is unique even among the large ultra-deep rift-formed lakes (such as Lake Tanganyika).  Baikal is fully saturated in oxygen down to its deepest depths.  The oxygen mixing throughout is due to currents caused by the inflowing rivers and exacerbated by lake storms.  These currents combine with currents caused by the earlier freeze of the northern part of the lake and the resultant temperature gradient forces more mixing.  The high level of oxygen removes oxygen level as a limit to growth. 

 

Some scientists have claimed that Lake Baikal is so resilient that the small human settlements along its shore have no impact on the ecology of the lake.  The monitoring study we completed was an attempt to evaluate the accuracy of this assertion in the littoral zone of Lake Baikal, in the Southwest portion of the lake. The littoral zone (also called the intertidal area) is where the land and sea meet, between the high and low tide zones.

 

Monitoring of the bottom (benthic zone) of Lake Baikal has been conducted over the whole lake for the past fifty years.  Monitoring of the pelagic and shelf zones has received considerably less attention.  It is estimated that up to 70% of the species in Lake Baikal live in the top 20 meters.  The littoral expanse from the shoreline for most of the lake is up to twenty meters followed by an abyss with many crevices. 

 

Our area of focus was the Bol’shye Koty settlement, a two-hour hydroplane trip along the Angara River and Baikal from the city of Irkutsk, Russia.  We took samples from a one cubic meter area from two separate project areas: one sample site was in the littoral zone near the shore directly adjacent to the center of the human settlement and near the outflow of the Bol’shye Koty creek; the other was in the Chornaya Bay, another area in the littoral shore zone north of Bol’shye Koty and further (approximately one kilometer) from human settlement.

 

Bol’shye Koty is a settlement of approximately sixty homes on the Southeastern shoreline of Lake Baikal north of the outflow of Baikal to the Angara River.  The settlement has been populated since the seventeenth century, and has had a few noted anthropogenic environmental impacts, but similar to the other settlements along Baikal’s shores.  Some actions in the region may also have impacts on the Lake, though adequate study has not yet been completed.  For example, in 1982 a nuclear explosion was conducted underground in the Irkutsk region, reportedly not far from the lake, as an experiment to examine the meteorological effects and also to search for gas an oil reserves.  More locally, the Bol’shye Koty river has been heavily managed and altered by human impact.  In attempts to avert flooding, settlers have moved rocks lining the bottom of the river to the banks, causing channelization and increased speed of the stream.  The stream is often seen filled with trash and products that may affect the water quality of the stream.  The homes and hostels in the settlements are also making improvements such as flush toilets to attract more tourists to the area.  The sewage produced is piped into the lake, not far from the shore.  Many of the human impacts on the stream also make their way to Lake Baikal, but scientists have so far stated that the lake is resilient enough to handle current pollution inputs.

 

Part of the evidence supporting Lake Baikal’s resiliency has come from the action of the arthropods in the lake, which act as miniature filters, eating pollution and organic matter.  The gammarids act as small scavengers, and researchers have found that they can smell decaying meat at a distance of one kilometer.  Arthropods are found in a great variety of depths in the lake and contribute to the remarkable clarity – sixty meters in many areas.  There are 270-280 species of arthropods in Lake Baikal and 60% are in the littoral zone.  Thus the health of the gammarid populations is key to the clarity and resiliency of Lake Baikal.

 

Project Design

We designed the project with two main parameters.  We selected two sample sites – one close to Bol’shye Koty and one further away in the Chornaya Bay.  These sites were chosen for their geographical similarity with the exception of the human settlement at Bol’shye Koty.  We collected samples in the littoral zone throughout the day and night and searched for six different groups of fauna: planaria, gammarid, nematodes, heeralabedes (maggots), oligochaetes, and cottoid fish species.  Within the gammarid (Crustacean) populations we studied the specific species of Eulimnogammarus verrucosus (Gerstfeldt, 1858), Eulimnogammarus vittatus (Dybowsky, 1874), Eulimnogammarus marituji Bazikalova (discovered 1945)[1], Eulimnogammarus cyaneus[2] (Dybowsky, 1874) , Gmelinoides fasciatus (Stebbing, 1899), and Pallasea gerstfeldtii/cancellus (we did not distinguish between the species of Pallasea). Eulimnogammarus is the youngest genus in the lake, and its species are known to exhibit the most rapid evolutionary development.

 

We counted the numbers of each species from each sample, weighed the biomass of each individual both wet and dry (oven-dried for 60 minutes) and measured each individual’s length.  We also measured the temperature, oxygen level and pH of the water for each sample. Our samples were taken from August 4-August 15, 2003. 

 

Results

Counting and measuring the biomass of each species at each sample, we were able to determine the dominant species both in biomass and in number.  The most dominant group in biomass in the littoral zone near Bol’shye Koty were the gammarids.  Due to storms, we failed to take a comparative sample in the littoral zone of the Chornaya Bay. Still, gammarids were the most dominant and important species to our work, and we were able to take samples of gammarids from both Bol’shye Koty and Chornaya Bay for comparison.

 

Our most important results came as we further compared the species to species dominance with the gammarid population of each location.  We found that there was indeed a difference in species dominance in the two locations.  In Chornaya Bay where there is less anthropogenic influence, we found the Eulimnogammarus verucosus to be dominant both numerically and in biomass.  In the Bol’shye Koty samples, Gmelinoides fasciatus was numerically dominant, though not dominant in terms of biomass due to its small size.

 

Conclusion and Recommendations

The gammarid species dominant at the Bol’shye Koty location is one that is known to be comparatively tolerant of anthropogenic impact, whereas the species dominant at the Chornaya Bay site is more ecologically sensitive. This suggests that the environmental impact of small settlements such as Bol’shye Koty does have an effect on the littoral zone of Lake Baikal. We recommend conducting a more precise analysis of how competition impacts population dynamics in both near-settlement and settlement-free littoral zone areas.



[1] http://www.imv.uit.no/amphipod/Baikal.htm

[2] This species is an attractive model for micro-evolutionary studies since it inhabits a very narrow zone a few meters wide, and 2 000 kilometers long. (http://aslo.org/phd/dialog/1995January-37.html)