References

geomorf

Геоморфология и палеогеография

Geomorfologiya i Paleogeografiya

2949-17892949-1797

10.15356/0435-4281-2012-4-64-72

geomorf-628

Research Article

Научные сообщения

Short communications

ИЗМЕНЕНИЯ КЛИМАТА В ПОЗДНЕМ ГОЛОЦЕНЕ И РАЗВИТИЕ МОРСКИХ БЕРЕГОВ ЧЕРНОГО МОРЯ

THE LATE HOLOCENE CLIMATE CHANGE AND COASTAL EVOLUTION OF THE BLACK SEA

Каплин

П. А.

Kaplin

P. A.

lzhindarev@yandex.ru

Поротов

А. В.

Porotov

A. V.

lzhindarev@yandex.ru

Московский государственный университет, МоскваРоссияMoscow State University, MoscowRussian Federation

2012

24072015

Геоморфология

6472

2015

Каплин П.А., Поротов А.В.

Kaplin P.A., Porotov A.V.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://geomorphology.igras.ru/jour/article/view/628

В рельефе и прибрежно-морских отложениях позднеголоценовых морские террас Черноморского побережья отчетливо выражены следы ритмичности, прослеживающиеся в генерациях береговых валов, а также в прослоях торфяников, которые маркируют и "трансгрессивные" и "регрессивные" фазы трансгрессии за последние 5.0 тыс. лет. Неравномерный ход трансгрессии и стадийность в эволюции рельефа морского побережья рассматриваются как результат короткопериодных климатических колебаний, которые определяли не только изменения темпов подъема уровня, но и поступления осадочного материала в береговую зону и его переработку волнениями и течениями, т.е. влияли на бюджет наносов береговой зоны.

Ритмичность в морфоседиментационном развитии Азово-Черноморского побережья синхронна общеклиматическим изменениям позднего голоцена и этапам развития рельефа береговой зоны на побережьях Средиземного, Балтийского и Северного морей и Атлантического побережья Европы.

The morpho-sedimentary structure of the Late Holocene coastal marine terraces on the north-eastern coast of the Black Sea display the traces of rhythmic pattern which are reflected in the intercalated peat among the liman silty clay and in several generations of beach ridges. These sea level indicators mark both the transgressive and regressive phases of general transgression during the last 5000 y. The irregularity in transgressions and coastal development are regarded as the result of short-term climate fluctuation that determined not only the rate of sea level rise but the change of sediment supply and storm frequency, which governed the drastic variation of sediment budget in coastal zone. The rhythmical pattern in coastal evolution on the Black Sea littoral correlated with millennium scale climate change in Northern Hemisphere that have been reflected in various types of relief changes in the Mediterranean and North-Atlantic coasts of Europe.

моряморские берегаголоценизменения климатаЧерное море

late Holocenethe Black Seamarine terracesbeach landform

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The authors declare that there are no conflicts of interest present.