Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system
Background On Late Cretaceous Tethyan upwelling sediments from the Mishash/Ghareb Formation (Negev, Israel), bulk geochemical and biomarker analyses were performed to explain the high proportion of phosphates in the lower part and of organic matter (OM) preserved in upper parts of the studied sectio...
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| Veröffentlicht in: | Geochemical transactions GT 2015-04, Vol.16 (1), p.2-2, Article 2 |
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| creator | Alsenz, Heiko Illner, Peter Ashckenazi-Polivoda, Sarit Meilijson, Aaron Abramovich, Sigal Feinstein, Shimon Almogi-Labin, Ahuva Berner, Zsolt Püttmann, Wilhelm |
| description | Background
On Late Cretaceous Tethyan upwelling sediments from the Mishash/Ghareb Formation (Negev, Israel), bulk geochemical and biomarker analyses were performed to explain the high proportion of phosphates in the lower part and of organic matter (OM) preserved in upper parts of the studied section. The profile is composed of three facies types; the underlying Phosphate Member (PM), the Oil Shale Member (OSM) and the overlying Marl Member (MM).
Results
Total organic carbon (TOC) contents are highly variable over the whole profile reaching from 0.6% in the MM, to 24.5% in the OSM. Total iron (TFe) varies from 0.1% in the PM to 3.3% in the OSM. Total sulfur (TS) ranges between 0.1% in the MM and 3.4% in the OSM, resulting in a high C/S ratio of 6.5 in the OSM section. A mean proportion of 11.5% total phosphorus (TP) in the PM changed abruptly with the facies to a mean value of only 0.9% in the OSM and the MM.
The TOC/TOC
OR
ratios argue for a high bacterial sulfate reduction activity and in addition, results from fatty acid analyses indicate that the activity of sulfide-oxidizing activity of bacteria was high during deposition of the PM, while decreasing during the deposition of the OSM.
Conclusions
The upwelling conditions effected a high primary productivity and consequently the presence of abundant OM. This, in combination with high sulfate availability in the sediments of the PM resulted in a higher sulfide production due to the activity of sulfate-reducing bacteria. Iron availability was a limiting factor during the deposition of the whole section, affecting the incorporation of S into OM. This resulted in the preservation of a substantial part of OM against microbial degradation due to naturally-occurring sulfurization processes expressed by the high C/S ratio of 6.5 in the OSM.
Further, the abundant sulfide in the pore water supported the growth of sulfide-oxidizing bacteria promoting the deposition of P, which amounted to as much as 15% in the PM. These conditions changed drastically from the PM to the OSM, resulting in a significant reduction of the apatite precipitation and a high concentration of reactive S species reacting with the OM. |
| doi_str_mv | 10.1186/s12932-015-0017-1 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_pubme</sourceid><recordid>TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4422410</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A541470479</galeid><sourcerecordid>A541470479</sourcerecordid><originalsourceid>FETCH-LOGICAL-c670t-4c4d33b59753b3e7f55c64ed8820449519208c5986ff7c2c11d9e1086b7ad0373</originalsourceid><addsrcrecordid>eNqFkttu1DAQhiMEoqXwANwgS9yARIrHcezkBqlaQam0EhKHa8vrTHZdEnuxnR6eglfGYUvpIhDyha2Zb357xn9RPAV6DNCI1xFYW7GSQl1SCrKEe8UhcCFL3ghx_875oHgU43lmQAr6sDhgdctbBuyw-H6K3mxwtEYPBC9sh84g6X0gaYNksO4rWWG6RHQkTkOvE5KA3WSS9e7Vz1AuIf7KdnoOEe06st34uN3MqDZmGqdhl7I5S5ZzeBEwaYN-imTaXuKQr1mTeB0Tjo-LB70eIj652Y-KL-_efl68L5cfTs8WJ8vSCElTyQ3vqmpVt7KuVhXKvq6N4Ng1DaOctzW0jDambhvR99IwA9C1CLQRK6k7WsnqqHiz091OqxE7gy4FPahtsKMO18prq_Yzzm7U2l8ozhnjQLPAixuB4L9NGJMabTS5F-3mxhRIYFI0lZT_R0VDoalZBRl9_gd67qfg8iSyIK1E_rZW_qbWekBlXe_zE80sqk5qDlxSLttMHf-Fyqubv9s77G2O7xW83CvITMKrtNZTjOrs08d9FnasCT7GgP3t6ICq2ZxqZ06Vzalmc6q5uWd3Z35b8cuNGWA7IOaUW2O40_0_VX8AEAfu8Q</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1703694997</pqid></control><display><type>article</type><title>Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system</title><source>DOAJ Directory of Open Access Journals</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>PubMed Central Open Access</source><source>Springer Nature OA Free Journals</source><source>PubMed Central</source><source>Free Full-Text Journals in Chemistry</source><source>SpringerLink Journals - AutoHoldings</source><creator>Alsenz, Heiko ; Illner, Peter ; Ashckenazi-Polivoda, Sarit ; Meilijson, Aaron ; Abramovich, Sigal ; Feinstein, Shimon ; Almogi-Labin, Ahuva ; Berner, Zsolt ; Püttmann, Wilhelm</creator><creatorcontrib>Alsenz, Heiko ; Illner, Peter ; Ashckenazi-Polivoda, Sarit ; Meilijson, Aaron ; Abramovich, Sigal ; Feinstein, Shimon ; Almogi-Labin, Ahuva ; Berner, Zsolt ; Püttmann, Wilhelm</creatorcontrib><description>Background
On Late Cretaceous Tethyan upwelling sediments from the Mishash/Ghareb Formation (Negev, Israel), bulk geochemical and biomarker analyses were performed to explain the high proportion of phosphates in the lower part and of organic matter (OM) preserved in upper parts of the studied section. The profile is composed of three facies types; the underlying Phosphate Member (PM), the Oil Shale Member (OSM) and the overlying Marl Member (MM).
Results
Total organic carbon (TOC) contents are highly variable over the whole profile reaching from 0.6% in the MM, to 24.5% in the OSM. Total iron (TFe) varies from 0.1% in the PM to 3.3% in the OSM. Total sulfur (TS) ranges between 0.1% in the MM and 3.4% in the OSM, resulting in a high C/S ratio of 6.5 in the OSM section. A mean proportion of 11.5% total phosphorus (TP) in the PM changed abruptly with the facies to a mean value of only 0.9% in the OSM and the MM.
The TOC/TOC
OR
ratios argue for a high bacterial sulfate reduction activity and in addition, results from fatty acid analyses indicate that the activity of sulfide-oxidizing activity of bacteria was high during deposition of the PM, while decreasing during the deposition of the OSM.
Conclusions
The upwelling conditions effected a high primary productivity and consequently the presence of abundant OM. This, in combination with high sulfate availability in the sediments of the PM resulted in a higher sulfide production due to the activity of sulfate-reducing bacteria. Iron availability was a limiting factor during the deposition of the whole section, affecting the incorporation of S into OM. This resulted in the preservation of a substantial part of OM against microbial degradation due to naturally-occurring sulfurization processes expressed by the high C/S ratio of 6.5 in the OSM.
Further, the abundant sulfide in the pore water supported the growth of sulfide-oxidizing bacteria promoting the deposition of P, which amounted to as much as 15% in the PM. These conditions changed drastically from the PM to the OSM, resulting in a significant reduction of the apatite precipitation and a high concentration of reactive S species reacting with the OM.</description><identifier>ISSN: 1467-4866</identifier><identifier>EISSN: 1467-4866</identifier><identifier>DOI: 10.1186/s12932-015-0017-1</identifier><identifier>PMID: 25949212</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Environmental Chemistry ; Geochemistry ; Research Article</subject><ispartof>Geochemical transactions GT, 2015-04, Vol.16 (1), p.2-2, Article 2</ispartof><rights>Alsenz et al.; licensee Springer. 2015. This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( ), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver ( ) applies to the data made available in this article, unless otherwise stated.</rights><rights>COPYRIGHT 2015 BioMed Central Ltd.</rights><rights>Geochemical Transactions is a copyright of Springer, 2015.</rights><rights>Alsenz et al.; licensee Springer. 2015</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c670t-4c4d33b59753b3e7f55c64ed8820449519208c5986ff7c2c11d9e1086b7ad0373</citedby><cites>FETCH-LOGICAL-c670t-4c4d33b59753b3e7f55c64ed8820449519208c5986ff7c2c11d9e1086b7ad0373</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4422410/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4422410/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,864,885,27923,27924,41119,41487,42188,42556,51318,51575,53790,53792</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/25949212$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Alsenz, Heiko</creatorcontrib><creatorcontrib>Illner, Peter</creatorcontrib><creatorcontrib>Ashckenazi-Polivoda, Sarit</creatorcontrib><creatorcontrib>Meilijson, Aaron</creatorcontrib><creatorcontrib>Abramovich, Sigal</creatorcontrib><creatorcontrib>Feinstein, Shimon</creatorcontrib><creatorcontrib>Almogi-Labin, Ahuva</creatorcontrib><creatorcontrib>Berner, Zsolt</creatorcontrib><creatorcontrib>Püttmann, Wilhelm</creatorcontrib><title>Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system</title><title>Geochemical transactions GT</title><addtitle>Geochem Trans</addtitle><addtitle>Geochem Trans</addtitle><description>Background
On Late Cretaceous Tethyan upwelling sediments from the Mishash/Ghareb Formation (Negev, Israel), bulk geochemical and biomarker analyses were performed to explain the high proportion of phosphates in the lower part and of organic matter (OM) preserved in upper parts of the studied section. The profile is composed of three facies types; the underlying Phosphate Member (PM), the Oil Shale Member (OSM) and the overlying Marl Member (MM).
Results
Total organic carbon (TOC) contents are highly variable over the whole profile reaching from 0.6% in the MM, to 24.5% in the OSM. Total iron (TFe) varies from 0.1% in the PM to 3.3% in the OSM. Total sulfur (TS) ranges between 0.1% in the MM and 3.4% in the OSM, resulting in a high C/S ratio of 6.5 in the OSM section. A mean proportion of 11.5% total phosphorus (TP) in the PM changed abruptly with the facies to a mean value of only 0.9% in the OSM and the MM.
The TOC/TOC
OR
ratios argue for a high bacterial sulfate reduction activity and in addition, results from fatty acid analyses indicate that the activity of sulfide-oxidizing activity of bacteria was high during deposition of the PM, while decreasing during the deposition of the OSM.
Conclusions
The upwelling conditions effected a high primary productivity and consequently the presence of abundant OM. This, in combination with high sulfate availability in the sediments of the PM resulted in a higher sulfide production due to the activity of sulfate-reducing bacteria. Iron availability was a limiting factor during the deposition of the whole section, affecting the incorporation of S into OM. This resulted in the preservation of a substantial part of OM against microbial degradation due to naturally-occurring sulfurization processes expressed by the high C/S ratio of 6.5 in the OSM.
Further, the abundant sulfide in the pore water supported the growth of sulfide-oxidizing bacteria promoting the deposition of P, which amounted to as much as 15% in the PM. These conditions changed drastically from the PM to the OSM, resulting in a significant reduction of the apatite precipitation and a high concentration of reactive S species reacting with the OM.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Chemistry</subject><subject>Geochemistry</subject><subject>Research Article</subject><issn>1467-4866</issn><issn>1467-4866</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkttu1DAQhiMEoqXwANwgS9yARIrHcezkBqlaQam0EhKHa8vrTHZdEnuxnR6eglfGYUvpIhDyha2Zb357xn9RPAV6DNCI1xFYW7GSQl1SCrKEe8UhcCFL3ghx_875oHgU43lmQAr6sDhgdctbBuyw-H6K3mxwtEYPBC9sh84g6X0gaYNksO4rWWG6RHQkTkOvE5KA3WSS9e7Vz1AuIf7KdnoOEe06st34uN3MqDZmGqdhl7I5S5ZzeBEwaYN-imTaXuKQr1mTeB0Tjo-LB70eIj652Y-KL-_efl68L5cfTs8WJ8vSCElTyQ3vqmpVt7KuVhXKvq6N4Ng1DaOctzW0jDambhvR99IwA9C1CLQRK6k7WsnqqHiz091OqxE7gy4FPahtsKMO18prq_Yzzm7U2l8ozhnjQLPAixuB4L9NGJMabTS5F-3mxhRIYFI0lZT_R0VDoalZBRl9_gd67qfg8iSyIK1E_rZW_qbWekBlXe_zE80sqk5qDlxSLttMHf-Fyqubv9s77G2O7xW83CvITMKrtNZTjOrs08d9FnasCT7GgP3t6ICq2ZxqZ06Vzalmc6q5uWd3Z35b8cuNGWA7IOaUW2O40_0_VX8AEAfu8Q</recordid><startdate>20150410</startdate><enddate>20150410</enddate><creator>Alsenz, Heiko</creator><creator>Illner, Peter</creator><creator>Ashckenazi-Polivoda, Sarit</creator><creator>Meilijson, Aaron</creator><creator>Abramovich, Sigal</creator><creator>Feinstein, Shimon</creator><creator>Almogi-Labin, Ahuva</creator><creator>Berner, Zsolt</creator><creator>Püttmann, Wilhelm</creator><general>Springer International Publishing</general><general>BioMed Central Ltd</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>3V.</scope><scope>7UA</scope><scope>7X7</scope><scope>7XB</scope><scope>8FE</scope><scope>8FG</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>L.G</scope><scope>L6V</scope><scope>M0S</scope><scope>M7S</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>7X8</scope><scope>7TG</scope><scope>7TN</scope><scope>KL.</scope><scope>5PM</scope></search><sort><creationdate>20150410</creationdate><title>Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system</title><author>Alsenz, Heiko ; Illner, Peter ; Ashckenazi-Polivoda, Sarit ; Meilijson, Aaron ; Abramovich, Sigal ; Feinstein, Shimon ; Almogi-Labin, Ahuva ; Berner, Zsolt ; Püttmann, Wilhelm</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c670t-4c4d33b59753b3e7f55c64ed8820449519208c5986ff7c2c11d9e1086b7ad0373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Chemistry</topic><topic>Geochemistry</topic><topic>Research Article</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Alsenz, Heiko</creatorcontrib><creatorcontrib>Illner, Peter</creatorcontrib><creatorcontrib>Ashckenazi-Polivoda, Sarit</creatorcontrib><creatorcontrib>Meilijson, Aaron</creatorcontrib><creatorcontrib>Abramovich, Sigal</creatorcontrib><creatorcontrib>Feinstein, Shimon</creatorcontrib><creatorcontrib>Almogi-Labin, Ahuva</creatorcontrib><creatorcontrib>Berner, Zsolt</creatorcontrib><creatorcontrib>Püttmann, Wilhelm</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>ProQuest Central (Corporate)</collection><collection>Water Resources Abstracts</collection><collection>Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection (ProQuest)</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>MEDLINE - Academic</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Geochemical transactions GT</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Alsenz, Heiko</au><au>Illner, Peter</au><au>Ashckenazi-Polivoda, Sarit</au><au>Meilijson, Aaron</au><au>Abramovich, Sigal</au><au>Feinstein, Shimon</au><au>Almogi-Labin, Ahuva</au><au>Berner, Zsolt</au><au>Püttmann, Wilhelm</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system</atitle><jtitle>Geochemical transactions GT</jtitle><stitle>Geochem Trans</stitle><addtitle>Geochem Trans</addtitle><date>2015-04-10</date><risdate>2015</risdate><volume>16</volume><issue>1</issue><spage>2</spage><epage>2</epage><pages>2-2</pages><artnum>2</artnum><issn>1467-4866</issn><eissn>1467-4866</eissn><abstract>Background
On Late Cretaceous Tethyan upwelling sediments from the Mishash/Ghareb Formation (Negev, Israel), bulk geochemical and biomarker analyses were performed to explain the high proportion of phosphates in the lower part and of organic matter (OM) preserved in upper parts of the studied section. The profile is composed of three facies types; the underlying Phosphate Member (PM), the Oil Shale Member (OSM) and the overlying Marl Member (MM).
Results
Total organic carbon (TOC) contents are highly variable over the whole profile reaching from 0.6% in the MM, to 24.5% in the OSM. Total iron (TFe) varies from 0.1% in the PM to 3.3% in the OSM. Total sulfur (TS) ranges between 0.1% in the MM and 3.4% in the OSM, resulting in a high C/S ratio of 6.5 in the OSM section. A mean proportion of 11.5% total phosphorus (TP) in the PM changed abruptly with the facies to a mean value of only 0.9% in the OSM and the MM.
The TOC/TOC
OR
ratios argue for a high bacterial sulfate reduction activity and in addition, results from fatty acid analyses indicate that the activity of sulfide-oxidizing activity of bacteria was high during deposition of the PM, while decreasing during the deposition of the OSM.
Conclusions
The upwelling conditions effected a high primary productivity and consequently the presence of abundant OM. This, in combination with high sulfate availability in the sediments of the PM resulted in a higher sulfide production due to the activity of sulfate-reducing bacteria. Iron availability was a limiting factor during the deposition of the whole section, affecting the incorporation of S into OM. This resulted in the preservation of a substantial part of OM against microbial degradation due to naturally-occurring sulfurization processes expressed by the high C/S ratio of 6.5 in the OSM.
Further, the abundant sulfide in the pore water supported the growth of sulfide-oxidizing bacteria promoting the deposition of P, which amounted to as much as 15% in the PM. These conditions changed drastically from the PM to the OSM, resulting in a significant reduction of the apatite precipitation and a high concentration of reactive S species reacting with the OM.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>25949212</pmid><doi>10.1186/s12932-015-0017-1</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences Environmental Chemistry Geochemistry Research Article |
| title | Geochemical evidence for the link between sulfate reduction, sulfide oxidation and phosphate accumulation in a Late Cretaceous upwelling system |
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