Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments

Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Ergin, M. [verfasserIn]

Format:	Artikel
Sprache:	Englisch

Erschienen:	1995

Schlagwörter:	Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling

Anmerkung:	© Springer-Verlag 1995

Übergeordnetes Werk:	Enthalten in: Geo-marine letters - Springer-Verlag, 1981, 15(1995), 1 vom: März, Seite 51-58
Übergeordnetes Werk:	volume:15 ; year:1995 ; number:1 ; month:03 ; pages:51-58

Links:	Volltext

DOI / URN:	10.1007/BF01204498

Katalog-ID:	OLC2036168523

Internformat


LEADER	01000caa a22002652 4500
001	OLC2036168523
003	DE-627
005	20230331143656.0
007	tu
008	200819s1995 xx \|\|\|\|\| 00\| \|\|eng c
024	7		\|a 10.1007/BF01204498 \|2 doi
035			\|a (DE-627)OLC2036168523
035			\|a (DE-He213)BF01204498-p
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
082	0	4	\|a 550 \|q VZ
082	0	4	\|a 550 \|q VZ
084			\|a 13 \|2 ssgn
100	1		\|a Ergin, M. \|e verfasserin \|4 aut
245	1	0	\|a Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
264		1	\|c 1995
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 © Springer-Verlag 1995
520			\|a Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation.
650		4	\|a Deep Water
650		4	\|a Bottom Sediment
650		4	\|a Depositional Environment
650		4	\|a Recent Sediment
650		4	\|a Redox Cycling
773	0	8	\|i Enthalten in \|t Geo-marine letters \|d Springer-Verlag, 1981 \|g 15(1995), 1 vom: März, Seite 51-58 \|w (DE-627)129932140 \|w (DE-600)381526-2 \|w (DE-576)015466973 \|x 0276-0460 \|7 nnns
773	1	8	\|g volume:15 \|g year:1995 \|g number:1 \|g month:03 \|g pages:51-58
856	4	1	\|u https://doi.org/10.1007/BF01204498 \|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_11
912			\|a GBV_ILN_21
912			\|a GBV_ILN_40
912			\|a GBV_ILN_62
912			\|a GBV_ILN_70
912			\|a GBV_ILN_600
912			\|a GBV_ILN_612
912			\|a GBV_ILN_2018
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4277
951			\|a AR
952			\|d 15 \|j 1995 \|e 1 \|c 03 \|h 51-58

Indexfelder

author_variant	m e me
matchkey_str	article:02760460:1995----::fetofnganienitiuinfnnhloadepaebakesdmnscmaiobtenx
hierarchy_sort_str	1995
publishDate	1995
allfields	10.1007/BF01204498 doi (DE-627)OLC2036168523 (DE-He213)BF01204498-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ergin, M. verfasserin aut Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1995 Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling Enthalten in Geo-marine letters Springer-Verlag, 1981 15(1995), 1 vom: März, Seite 51-58 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:15 year:1995 number:1 month:03 pages:51-58 https://doi.org/10.1007/BF01204498 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 15 1995 1 03 51-58
spelling	10.1007/BF01204498 doi (DE-627)OLC2036168523 (DE-He213)BF01204498-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ergin, M. verfasserin aut Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1995 Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling Enthalten in Geo-marine letters Springer-Verlag, 1981 15(1995), 1 vom: März, Seite 51-58 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:15 year:1995 number:1 month:03 pages:51-58 https://doi.org/10.1007/BF01204498 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 15 1995 1 03 51-58
allfields_unstemmed	10.1007/BF01204498 doi (DE-627)OLC2036168523 (DE-He213)BF01204498-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ergin, M. verfasserin aut Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1995 Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling Enthalten in Geo-marine letters Springer-Verlag, 1981 15(1995), 1 vom: März, Seite 51-58 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:15 year:1995 number:1 month:03 pages:51-58 https://doi.org/10.1007/BF01204498 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 15 1995 1 03 51-58
allfieldsGer	10.1007/BF01204498 doi (DE-627)OLC2036168523 (DE-He213)BF01204498-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ergin, M. verfasserin aut Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1995 Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling Enthalten in Geo-marine letters Springer-Verlag, 1981 15(1995), 1 vom: März, Seite 51-58 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:15 year:1995 number:1 month:03 pages:51-58 https://doi.org/10.1007/BF01204498 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 15 1995 1 03 51-58
allfieldsSound	10.1007/BF01204498 doi (DE-627)OLC2036168523 (DE-He213)BF01204498-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ergin, M. verfasserin aut Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1995 Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling Enthalten in Geo-marine letters Springer-Verlag, 1981 15(1995), 1 vom: März, Seite 51-58 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:15 year:1995 number:1 month:03 pages:51-58 https://doi.org/10.1007/BF01204498 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 15 1995 1 03 51-58
language	English
source	Enthalten in Geo-marine letters 15(1995), 1 vom: März, Seite 51-58 volume:15 year:1995 number:1 month:03 pages:51-58
sourceStr	Enthalten in Geo-marine letters 15(1995), 1 vom: März, Seite 51-58 volume:15 year:1995 number:1 month:03 pages:51-58
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling
dewey-raw	550
isfreeaccess_bool	false
container_title	Geo-marine letters
authorswithroles_txt_mv	Ergin, M. @@aut@@
publishDateDaySort_date	1995-03-01T00:00:00Z
hierarchy_top_id	129932140
dewey-sort	3550
id	OLC2036168523
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">OLC2036168523</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230331143656.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1995 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF01204498</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2036168523</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF01204498-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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ergin, M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1995</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">© Springer-Verlag 1995</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Deep Water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Bottom Sediment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Depositional Environment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Recent Sediment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Redox Cycling</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geo-marine letters</subfield><subfield code="d">Springer-Verlag, 1981</subfield><subfield code="g">15(1995), 1 vom: März, Seite 51-58</subfield><subfield code="w">(DE-627)129932140</subfield><subfield code="w">(DE-600)381526-2</subfield><subfield code="w">(DE-576)015466973</subfield><subfield code="x">0276-0460</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:1995</subfield><subfield code="g">number:1</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:51-58</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF01204498</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_600</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_612</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">15</subfield><subfield code="j">1995</subfield><subfield code="e">1</subfield><subfield code="c">03</subfield><subfield code="h">51-58</subfield></datafield></record></collection>
author	Ergin, M.
spellingShingle	Ergin, M. ddc 550 ssgn 13 misc Deep Water misc Bottom Sediment misc Depositional Environment misc Recent Sediment misc Redox Cycling Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
authorStr	Ergin, M.
ppnlink_with_tag_str_mv	@@773@@(DE-627)129932140
format	Article
dewey-ones	550 - Earth sciences
delete_txt_mv	keep
author_role	aut
collection	OLC
remote_str	false
illustrated	Not Illustrated
issn	0276-0460
topic_title	550 VZ 13 ssgn Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments Deep Water Bottom Sediment Depositional Environment Recent Sediment Redox Cycling
topic	ddc 550 ssgn 13 misc Deep Water misc Bottom Sediment misc Depositional Environment misc Recent Sediment misc Redox Cycling
topic_unstemmed	ddc 550 ssgn 13 misc Deep Water misc Bottom Sediment misc Depositional Environment misc Recent Sediment misc Redox Cycling
topic_browse	ddc 550 ssgn 13 misc Deep Water misc Bottom Sediment misc Depositional Environment misc Recent Sediment misc Redox Cycling
format_facet	Aufsätze Gedruckte Aufsätze
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	nc
hierarchy_parent_title	Geo-marine letters
hierarchy_parent_id	129932140
dewey-tens	550 - Earth sciences & geology
hierarchy_top_title	Geo-marine letters
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)129932140 (DE-600)381526-2 (DE-576)015466973
title	Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
ctrlnum	(DE-627)OLC2036168523 (DE-He213)BF01204498-p
title_full	Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
author_sort	Ergin, M.
journal	Geo-marine letters
journalStr	Geo-marine letters
lang_code	eng
isOA_bool	false
dewey-hundreds	500 - Science
recordtype	marc
publishDateSort	1995
contenttype_str_mv	txt
container_start_page	51
author_browse	Ergin, M.
container_volume	15
class	550 VZ 13 ssgn
format_se	Aufsätze
author-letter	Ergin, M.
doi_str_mv	10.1007/BF01204498
dewey-full	550
title_sort	effects of fine grain size on distribution of mn in shallow and deep water black sea sediments: a comparison between oxic and anoxic depositional environments
title_auth	Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
abstract	Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. © Springer-Verlag 1995
abstractGer	Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. © Springer-Verlag 1995
abstract_unstemmed	Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation. © Springer-Verlag 1995
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277
container_issue	1
title_short	Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments
url	https://doi.org/10.1007/BF01204498
remote_bool	false
ppnlink	129932140
mediatype_str_mv	n
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/BF01204498
up_date	2024-07-04T02:49:29.051Z
_version_	1803615070122409984
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">OLC2036168523</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230331143656.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1995 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF01204498</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2036168523</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF01204498-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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ergin, M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1995</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">© Springer-Verlag 1995</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The uppermost 5–6 cm of the sediments (between 8 and 2248 m water depths) were studied to understand the effects of varying redox conditions on the Mn distribution in the recent sediments of the Black Sea. It was found that most Mn concentrations are consistent with the average abundance in crustal and/or sedimentary rocks. There exist no important differences between Mn concentrations in oxic (shallower water; <70 m) and anoxic (deeper water; 120 m) sediments. Previously reported Mn-enrichment above the Black Sea oxic/anoxic interface, due to the peculiar redox cycling, shows no significant contribution of Mn to the bottom sediments. A marked relationship between total Mn concentrations and clay/mud contents at shelf depth along the southern Black Sea margin indicates increased accumulation of Mn in association with the fine-grained particles and eastward water circulation.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Deep Water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Bottom Sediment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Depositional Environment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Recent Sediment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Redox Cycling</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geo-marine letters</subfield><subfield code="d">Springer-Verlag, 1981</subfield><subfield code="g">15(1995), 1 vom: März, Seite 51-58</subfield><subfield code="w">(DE-627)129932140</subfield><subfield code="w">(DE-600)381526-2</subfield><subfield code="w">(DE-576)015466973</subfield><subfield code="x">0276-0460</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:1995</subfield><subfield code="g">number:1</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:51-58</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF01204498</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_600</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_612</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">15</subfield><subfield code="j">1995</subfield><subfield code="e">1</subfield><subfield code="c">03</subfield><subfield code="h">51-58</subfield></datafield></record></collection>
score	7.399295

Nicht das Richtige dabei?

Schreiben Sie uns!

Effects of fine grain size on distribution of Mn in shallow and deep water Black Sea sediments: A comparison between oxic and anoxic depositional environments

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?