Статья

Татьяна Андреевна Копотева, с.н.с., Институт водных и экологических проблем ДВО РАН (680000, г. Хабаровск, ул. Дикопольцева, д. 56); e-mail: kopoteva@ivep.as.khb.ru
Виктория Алексеевна Купцова, н.с., Институт водных и экологических проблем ДВО РАН (680000, г. Хабаровск, ул. Дикопольцева, д. 56); e-mail: victoria@ivep.as.khb.ru

Kopoteva T.A., Kuptsova V.A. 2019. Effects of pyrogenic factor on wetlands of Petrovskaya Pad' (Jewish Autonomous Region, Russia) // Nature Conservation Research. Vol. 4(Suppl.1). P. 35–44. https://dx.doi.org/10.24189/ncr.2019.034

В последние десятилетия по периферии заповедника Бастак в урочище Петровская падь сложилась тяжелая пирогенная обстановка, угрожающая территории заповедника. По материалам геоботанического обследования Петровской пади, сделанного в ходе совместной экспедиции в 2009 г., дается оценка современного состояния растительного покрова и постпирогенных изменений. В настоящее время этот район Среднеамурской низменности является ярким примером деградации водно-болотных угодий (ВБУ) в результате многократного воздействия палов, применяющихся в Приамурье населением и работниками сельского хозяйства. Отмечено широкое распространение процесса ксеризации растительности травяных болот из-за резкого снижения уровня грунтовых вод. Проанализированы материалы предыдущих исследователей, которые привели к выводу, что из растительного покрова территории полностью исчезли мезотрофные кустарничково-сфагновые болота, ранее описывавшиеся Г. Э. Куренцовой. Их деградация объясняется авторами постоянно действующим пирогенным фактором. Впервые приводятся данные динамики структуры акротельма в постпирогенный период, полученные в ходе девятилетнего мониторинга. Глубокие изменения в структуре акротельма приводят к тому, что восстановление мезотрофных болот занимает десятки лет.

акротельм, биоразнообразие, болота, неконтролируемые палы, пирогенный субклимакс

Поступила: 26.11.2018. Исправлена: 19.03.2019. Принята к опубликованию: 23.04.2019.

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