(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...
Main Authors: | , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2000
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.761701 https://doi.org/10.1594/PANGAEA.761701 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761701 |
---|---|
record_format |
openpolar |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761701 2023-05-15T14:24:40+02:00 (Table 3) Grain size composition of Holocene deposits from the Kara Sea Pavlidis, Yury A Shcherbakov, Fyodor A MEDIAN LATITUDE: 72.350000 * MEDIAN LONGITUDE: 59.125000 * SOUTH-BOUND LATITUDE: 72.190000 * WEST-BOUND LONGITUDE: 57.850000 * NORTH-BOUND LATITUDE: 72.510000 * EAST-BOUND LONGITUDE: 60.400000 * MINIMUM DEPTH, sediment/rock: 1.0 m * MAXIMUM DEPTH, sediment/rock: 202.5 m 2000-06-15 text/tab-separated-values, 64 data points https://doi.pangaea.de/10.1594/PANGAEA.761701 https://doi.org/10.1594/PANGAEA.761701 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.761701 https://doi.org/10.1594/PANGAEA.761701 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 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 Archive of Ocean Data ARCOD Depth bottom/max sediment/rock top/min Elevation of event Epoch Event label GC Grain size analysis after Petelin (1967 Nauka Moscow) Gravity corer Kara Sea Latitude of event Longitude of event Professor Shtokman PSh12 PSh12-1405 PSh12-1407 Size fraction < 0.001 mm clay Size fraction < 0.010 mm Size fraction > 1 mm gravel Size fraction 0.100-0.010 mm Size fraction 1-0.1 mm Dataset 2000 ftpangaea https://doi.org/10.1594/PANGAEA.761701 2023-01-20T08:52:21Z 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. Dataset Arctic Arctic Kara Sea PANGAEA - Data Publisher for Earth & Environmental Science Arctic Kara Sea ENVELOPE(57.850000,60.400000,72.510000,72.190000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Archive of Ocean Data ARCOD Depth bottom/max sediment/rock top/min Elevation of event Epoch Event label GC Grain size analysis after Petelin (1967 Nauka Moscow) Gravity corer Kara Sea Latitude of event Longitude of event Professor Shtokman PSh12 PSh12-1405 PSh12-1407 Size fraction < 0.001 mm clay Size fraction < 0.010 mm Size fraction > 1 mm gravel Size fraction 0.100-0.010 mm Size fraction 1-0.1 mm |
spellingShingle |
Archive of Ocean Data ARCOD Depth bottom/max sediment/rock top/min Elevation of event Epoch Event label GC Grain size analysis after Petelin (1967 Nauka Moscow) Gravity corer Kara Sea Latitude of event Longitude of event Professor Shtokman PSh12 PSh12-1405 PSh12-1407 Size fraction < 0.001 mm clay Size fraction < 0.010 mm Size fraction > 1 mm gravel Size fraction 0.100-0.010 mm Size fraction 1-0.1 mm Pavlidis, Yury A Shcherbakov, Fyodor A (Table 3) Grain size composition of Holocene deposits from the Kara Sea |
topic_facet |
Archive of Ocean Data ARCOD Depth bottom/max sediment/rock top/min Elevation of event Epoch Event label GC Grain size analysis after Petelin (1967 Nauka Moscow) Gravity corer Kara Sea Latitude of event Longitude of event Professor Shtokman PSh12 PSh12-1405 PSh12-1407 Size fraction < 0.001 mm clay Size fraction < 0.010 mm Size fraction > 1 mm gravel Size fraction 0.100-0.010 mm Size fraction 1-0.1 mm |
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. |
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://doi.pangaea.de/10.1594/PANGAEA.761701 https://doi.org/10.1594/PANGAEA.761701 |
op_coverage |
MEDIAN LATITUDE: 72.350000 * MEDIAN LONGITUDE: 59.125000 * SOUTH-BOUND LATITUDE: 72.190000 * WEST-BOUND LONGITUDE: 57.850000 * NORTH-BOUND LATITUDE: 72.510000 * EAST-BOUND LONGITUDE: 60.400000 * MINIMUM DEPTH, sediment/rock: 1.0 m * MAXIMUM DEPTH, sediment/rock: 202.5 m |
long_lat |
ENVELOPE(57.850000,60.400000,72.510000,72.190000) |
geographic |
Arctic Kara Sea |
geographic_facet |
Arctic Kara Sea |
genre |
Arctic Arctic Kara Sea |
genre_facet |
Arctic Arctic Kara Sea |
op_source |
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 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.761701 https://doi.org/10.1594/PANGAEA.761701 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.761701 |
_version_ |
1766297113016139776 |