(Table 3) Grain size composition of Holocene deposits from the Kara Sea ...

A new generalized schematic map of distribution of recent sediments within Eurasian Arctic shelves is considered. The sediments have accumulated as a result of interaction of various factors and processes specific to high latitudes. They include input of terrigenous material by modern glaciers, ice...

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Bibliographic Details
Main Authors: Pavlidis, Yury A, Shcherbakov, Fyodor A
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.761701
https://doi.pangaea.de/10.1594/PANGAEA.761701
id ftdatacite:10.1594/pangaea.761701
record_format openpolar
spelling ftdatacite:10.1594/pangaea.761701 2024-09-15T18:16:11+00:00 (Table 3) Grain size composition of Holocene deposits from the Kara Sea ... Pavlidis, Yury A Shcherbakov, Fyodor A 2000 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.761701 https://doi.pangaea.de/10.1594/PANGAEA.761701 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Epoch Size fraction > 1 mm, gravel Size fraction 1-0.1 mm Size fraction 0.100-0.010 mm Size fraction < 0.010 mm Size fraction < 0.001 mm, clay Gravity corer Grain size analysis after Petelin 1967, Nauka, Moscow PSh12 Professor Shtokman Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 2000 ftdatacite https://doi.org/10.1594/pangaea.761701 2024-08-01T10:54:59Z A new generalized schematic map of distribution of recent sediments within Eurasian Arctic shelves is considered. The sediments have accumulated as a result of interaction of various factors and processes specific to high latitudes. They include input of terrigenous material by modern glaciers, ice transport, thermal abrasion, sedimentation controlled by many years of ice cover, and others. Characteristic regularity is marked over Arctic shelves: in seas with heavier ice cover, the most fine-grained deposits are distributed, they contain minimum amount of coarse-grained ice rafted debris; in seas with lighter ice cover mosaic distribution of various types of sediments is observed. Composition of surface sediments from the Arctic shelves corresponds to a relatively cool stage of the modern interglacial period. In the 21-st century a new warming is expected. ... : Supplement to: Pavlidis, Yury A; Shcherbakov, Fyodor A (2000): Recent bottom sediments of the Eurasian Arctic Seas. Translated from Okeanologiya, 2000, 40(1), 137-147, Oceanology, 40(1), 129-138 ... Dataset Kara Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
Elevation of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Epoch
Size fraction > 1 mm, gravel
Size fraction 1-0.1 mm
Size fraction 0.100-0.010 mm
Size fraction < 0.010 mm
Size fraction < 0.001 mm, clay
Gravity corer
Grain size analysis after Petelin 1967, Nauka, Moscow
PSh12
Professor Shtokman
Archive of Ocean Data ARCOD
spellingShingle Event label
Latitude of event
Longitude of event
Elevation of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Epoch
Size fraction > 1 mm, gravel
Size fraction 1-0.1 mm
Size fraction 0.100-0.010 mm
Size fraction < 0.010 mm
Size fraction < 0.001 mm, clay
Gravity corer
Grain size analysis after Petelin 1967, Nauka, Moscow
PSh12
Professor Shtokman
Archive of Ocean Data ARCOD
Pavlidis, Yury A
Shcherbakov, Fyodor A
(Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
topic_facet Event label
Latitude of event
Longitude of event
Elevation of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Epoch
Size fraction > 1 mm, gravel
Size fraction 1-0.1 mm
Size fraction 0.100-0.010 mm
Size fraction < 0.010 mm
Size fraction < 0.001 mm, clay
Gravity corer
Grain size analysis after Petelin 1967, Nauka, Moscow
PSh12
Professor Shtokman
Archive of Ocean Data ARCOD
description A new generalized schematic map of distribution of recent sediments within Eurasian Arctic shelves is considered. The sediments have accumulated as a result of interaction of various factors and processes specific to high latitudes. They include input of terrigenous material by modern glaciers, ice transport, thermal abrasion, sedimentation controlled by many years of ice cover, and others. Characteristic regularity is marked over Arctic shelves: in seas with heavier ice cover, the most fine-grained deposits are distributed, they contain minimum amount of coarse-grained ice rafted debris; in seas with lighter ice cover mosaic distribution of various types of sediments is observed. Composition of surface sediments from the Arctic shelves corresponds to a relatively cool stage of the modern interglacial period. In the 21-st century a new warming is expected. ... : Supplement to: Pavlidis, Yury A; Shcherbakov, Fyodor A (2000): Recent bottom sediments of the Eurasian Arctic Seas. Translated from Okeanologiya, 2000, 40(1), 137-147, Oceanology, 40(1), 129-138 ...
format Dataset
author Pavlidis, Yury A
Shcherbakov, Fyodor A
author_facet Pavlidis, Yury A
Shcherbakov, Fyodor A
author_sort Pavlidis, Yury A
title (Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
title_short (Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
title_full (Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
title_fullStr (Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
title_full_unstemmed (Table 3) Grain size composition of Holocene deposits from the Kara Sea ...
title_sort (table 3) grain size composition of holocene deposits from the kara sea ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.761701
https://doi.pangaea.de/10.1594/PANGAEA.761701
genre Kara Sea
genre_facet Kara Sea
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.761701
_version_ 1810454200218288128