Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and oc...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Matul, A. G. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Pleiades Publishing, Inc. 2015 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Oceanology - Pleiades Publishing, 1966, 55(2015), 1 vom: Feb., Seite 91-99 |
|---|---|
| Übergeordnetes Werk: |
volume:55 ; year:2015 ; number:1 ; month:02 ; pages:91-99 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0001437015010130 |
|---|
| Katalog-ID: |
OLC2071618114 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2071618114 | ||
| 003 | DE-627 | ||
| 005 | 20230302141628.0 | ||
| 007 | tu | ||
| 008 | 200819s2015 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1134/S0001437015010130 |2 doi | |
| 035 | |a (DE-627)OLC2071618114 | ||
| 035 | |a (DE-He213)S0001437015010130-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 14 |2 ssgn | ||
| 100 | 1 | |a Matul, A. G. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| 264 | 1 | |c 2015 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Pleiades Publishing, Inc. 2015 | ||
| 520 | |a Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. | ||
| 650 | 4 | |a Last Glacial Maximum | |
| 650 | 4 | |a Glacial Maximum | |
| 650 | 4 | |a Intermediate Water | |
| 650 | 4 | |a Radiolaria | |
| 650 | 4 | |a Lithostratigraphy | |
| 700 | 1 | |a Abelmann, A. |4 aut | |
| 700 | 1 | |a Gersonde, R. |4 aut | |
| 700 | 1 | |a Nürnberg, D. |4 aut | |
| 700 | 1 | |a Tiedemann, R. |4 aut | |
| 700 | 1 | |a Kruglikova, S. B. |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Oceanology |d Pleiades Publishing, 1966 |g 55(2015), 1 vom: Feb., Seite 91-99 |w (DE-627)130005363 |w (DE-600)417045-3 |w (DE-576)9130005361 |x 0001-4370 |7 nnns |
| 773 | 1 | 8 | |g volume:55 |g year:2015 |g number:1 |g month:02 |g pages:91-99 |
| 856 | 4 | 1 | |u https://doi.org/10.1134/S0001437015010130 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_201 | ||
| 951 | |a AR | ||
| 952 | |d 55 |j 2015 |e 1 |c 02 |h 91-99 | ||
| author_variant |
a g m ag agm a a aa r g rg d n dn r t rt s b k sb sbk |
|---|---|
| matchkey_str |
article:00014370:2015----::aeutrayitiuinfhccaohrdvsaaailraseiselcinfosbeetltooteotpcfcn |
| hierarchy_sort_str |
2015 |
| publishDate |
2015 |
| allfields |
10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
| spelling |
10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
| allfields_unstemmed |
10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
| allfieldsGer |
10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
| allfieldsSound |
10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
| language |
English |
| source |
Enthalten in Oceanology 55(2015), 1 vom: Feb., Seite 91-99 volume:55 year:2015 number:1 month:02 pages:91-99 |
| sourceStr |
Enthalten in Oceanology 55(2015), 1 vom: Feb., Seite 91-99 volume:55 year:2015 number:1 month:02 pages:91-99 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Oceanology |
| authorswithroles_txt_mv |
Matul, A. G. @@aut@@ Abelmann, A. @@aut@@ Gersonde, R. @@aut@@ Nürnberg, D. @@aut@@ Tiedemann, R. @@aut@@ Kruglikova, S. B. @@aut@@ |
| publishDateDaySort_date |
2015-02-01T00:00:00Z |
| hierarchy_top_id |
130005363 |
| dewey-sort |
3550 |
| id |
OLC2071618114 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2071618114</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230302141628.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S0001437015010130</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2071618114</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S0001437015010130-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Matul, A. G.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Inc. 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Last Glacial Maximum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Glacial Maximum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Intermediate Water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiolaria</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lithostratigraphy</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Abelmann, A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gersonde, R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nürnberg, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tiedemann, R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kruglikova, S. B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Oceanology</subfield><subfield code="d">Pleiades Publishing, 1966</subfield><subfield code="g">55(2015), 1 vom: Feb., Seite 91-99</subfield><subfield code="w">(DE-627)130005363</subfield><subfield code="w">(DE-600)417045-3</subfield><subfield code="w">(DE-576)9130005361</subfield><subfield code="x">0001-4370</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:55</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:1</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:91-99</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0001437015010130</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_201</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">55</subfield><subfield code="j">2015</subfield><subfield code="e">1</subfield><subfield code="c">02</subfield><subfield code="h">91-99</subfield></datafield></record></collection>
|
| author |
Matul, A. G. |
| spellingShingle |
Matul, A. G. ddc 550 ssgn 14 misc Last Glacial Maximum misc Glacial Maximum misc Intermediate Water misc Radiolaria misc Lithostratigraphy Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| authorStr |
Matul, A. G. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)130005363 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0001-4370 |
| topic_title |
550 VZ 14 ssgn Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy |
| topic |
ddc 550 ssgn 14 misc Last Glacial Maximum misc Glacial Maximum misc Intermediate Water misc Radiolaria misc Lithostratigraphy |
| topic_unstemmed |
ddc 550 ssgn 14 misc Last Glacial Maximum misc Glacial Maximum misc Intermediate Water misc Radiolaria misc Lithostratigraphy |
| topic_browse |
ddc 550 ssgn 14 misc Last Glacial Maximum misc Glacial Maximum misc Intermediate Water misc Radiolaria misc Lithostratigraphy |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Oceanology |
| hierarchy_parent_id |
130005363 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Oceanology |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 |
| title |
Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| ctrlnum |
(DE-627)OLC2071618114 (DE-He213)S0001437015010130-p |
| title_full |
Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| author_sort |
Matul, A. G. |
| journal |
Oceanology |
| journalStr |
Oceanology |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2015 |
| contenttype_str_mv |
txt |
| container_start_page |
91 |
| author_browse |
Matul, A. G. Abelmann, A. Gersonde, R. Nürnberg, D. Tiedemann, R. Kruglikova, S. B. |
| container_volume |
55 |
| class |
550 VZ 14 ssgn |
| format_se |
Aufsätze |
| author-letter |
Matul, A. G. |
| doi_str_mv |
10.1134/S0001437015010130 |
| dewey-full |
550 |
| title_sort |
late quaternary distribution of the cycladophora davisiana radiolarian species: reflection of possible ventilation of the north pacific intermediate water during the last glacial maximum |
| title_auth |
Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| abstract |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
| abstractGer |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
| abstract_unstemmed |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 |
| container_issue |
1 |
| title_short |
Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
| url |
https://doi.org/10.1134/S0001437015010130 |
| remote_bool |
false |
| author2 |
Abelmann, A. Gersonde, R. Nürnberg, D. Tiedemann, R. Kruglikova, S. B. |
| author2Str |
Abelmann, A. Gersonde, R. Nürnberg, D. Tiedemann, R. Kruglikova, S. B. |
| ppnlink |
130005363 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1134/S0001437015010130 |
| up_date |
2024-07-04T03:51:15.804Z |
| _version_ |
1803618956935692288 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2071618114</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230302141628.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S0001437015010130</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2071618114</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S0001437015010130-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Matul, A. G.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Inc. 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Last Glacial Maximum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Glacial Maximum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Intermediate Water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiolaria</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lithostratigraphy</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Abelmann, A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gersonde, R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nürnberg, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tiedemann, R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kruglikova, S. B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Oceanology</subfield><subfield code="d">Pleiades Publishing, 1966</subfield><subfield code="g">55(2015), 1 vom: Feb., Seite 91-99</subfield><subfield code="w">(DE-627)130005363</subfield><subfield code="w">(DE-600)417045-3</subfield><subfield code="w">(DE-576)9130005361</subfield><subfield code="x">0001-4370</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:55</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:1</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:91-99</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0001437015010130</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_201</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">55</subfield><subfield code="j">2015</subfield><subfield code="e">1</subfield><subfield code="c">02</subfield><subfield code="h">91-99</subfield></datafield></record></collection>
|
| score |
7.3995314 |