LATE HOLOCENE SEDIMENTARY RESPONSE TO SOLAR AND COSMIC RAY ACTIVITY INFLUENCED CLIMATE VARIABILITY IN THE NE PACIFIC

dc.contributor.author	Patterson R.T.
dc.contributor.author	Chang A.
dc.contributor.author	Prokoph A.
dc.date.accessioned	2022-11-11T08:24:03Z
dc.date.available	2022-11-11T08:24:03Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=14591030
dc.identifier.citation	Sedimentary Geology, 2004, 172, 1-2, 67-84
dc.identifier.issn	0037-0738
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/39626
dc.description.abstract	Marine-laminated sediments along the NE Pacific coast (Effingham inlet, Vancouver Island) provide an archive of climate variability at annual to millennial scales. A 7.75-m portion of piston core TUL99B-03 was deposited during a ∼3045-year interval [∼1440–4485 years before present (yBP)] under primarily anoxic conditions. Darker clay laminae were deposited under higher precipitation conditions in winter, and diatom-dominated laminae were laid down when marine productivity was higher in the spring through autumn.
dc.subject	NE Pacific
dc.subject	Laminated sediments
dc.subject	Wavelet transform
dc.subject	Cyclicity
dc.subject	Solar irradiance
dc.subject	Climate change
dc.title	LATE HOLOCENE SEDIMENTARY RESPONSE TO SOLAR AND COSMIC RAY ACTIVITY INFLUENCED CLIMATE VARIABILITY IN THE NE PACIFIC
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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