Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22
Through the Deep Sea Drilling Project samples of interstitial solutions of deeply buried marine sediments throughout the World Ocean have been obtained and analyzed. The studies have shown that in all but the most slowly deposited sediments pore fluids exhibit changes in composition upon burial. The...
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1975
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.706822 2024-09-09T19:56:17+00:00 Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 Sayles, Frederick L Manheim, Frank T MEDIAN LATITUDE: 18.161913 * MEDIAN LONGITUDE: -142.984900 * SOUTH-BOUND LATITUDE: -11.336800 * WEST-BOUND LONGITUDE: 88.718000 * NORTH-BOUND LATITUDE: 57.496000 * EAST-BOUND LONGITUDE: -7.974800 * DATE/TIME START: 1969-07-03T00:00:00 * DATE/TIME END: 1972-02-24T00:00:00 1975 application/zip, 15 datasets https://doi.pangaea.de/10.1594/PANGAEA.706822 https://doi.org/10.1594/PANGAEA.706822 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.706822 https://doi.org/10.1594/PANGAEA.706822 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Sayles, Frederick L; Manheim, Frank T (1975): Interstitial solutions and diagenesis in deeply buried marine sediments: results from the Deep Sea Drilling Project. Geochimica et Cosmochimica Acta, 39(2), 103-127, https://doi.org/10.1016/0016-7037(75)90165-9 11-102 12-116 12-119 14-137 15-147 15-149 22-214 22-216 22-217 6-50 6-51 6-55 7-66 8-70 8-71 Caribbean Sea/BASIN Caribbean Sea/RIDGE Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Indian Ocean//RIDGE Leg11 Leg12 Leg14 Leg15 Leg22 Leg6 Leg7 Leg8 North Atlantic/BASIN North Atlantic/HILL North Atlantic/RIDGE North Atlantic/SEAMOUNT North Pacific/BASIN North Pacific/CONT RISE North Pacific/PLAIN North Pacific/RIDGE dataset publication series 1975 ftpangaea https://doi.org/10.1594/PANGAEA.70682210.1016/0016-7037(75)90165-9 2024-07-24T02:31:42Z Through the Deep Sea Drilling Project samples of interstitial solutions of deeply buried marine sediments throughout the World Ocean have been obtained and analyzed. The studies have shown that in all but the most slowly deposited sediments pore fluids exhibit changes in composition upon burial. These changes can be grouped into a few consistent patterns that facilitate identification of the diagenetic reactions occurring in the sediments. Pelagic clays and slowly deposited (<1 cm/1000 yr) biogenic sediments are the only types that exhibit little evidence of reaction in the pore waters. In most biogenic sediments sea water undergoes considerable alteration. In sediments deposited at rates up to a few cm/1000 yr the changes chiefly involve gains of Ca(2+) and Sr(2+) and losses of Mg(2+) which balance the Ca(2+) enrichment. The Ca-Mg substitution may often reach 30 mM/kg while Sr(2+) may be enriched 15-fold over sea water. These changes reflect recrystallization of biogenic calcite and the substitution of Mg(2+) for Ca(2+) during this reaction. The Ca-Mg-carbonate formed is most likely a dolomitic phase. A related but more complex pattern is found in carbonate sediments deposited at somewhat greater rates. Ca(2+) and Sr(2+) enrichment is again characteristic, but Mg(2+) losses exceed Ca(2+) gains with the excess being balanced by SO4(post staggered 2-) losses. The data indicate that the reactions are similar to those noted above, except that the Ca(2+) released is not kept in solution but is precipitated by the HCO3(post staggered -) produced in SO4(post staggered 2-) reduction. In both these types of pore waters Na(+) is usually conservative, but K(+) depletions are frequent. In several partly consolidated sediment sections approaching igneous basement contact, very marked interstitial calcium enrichment has been found (to 5.5 g/kg). These phenomena are marked by pronounced depletion in Na(+), Si and CO2, and slight enhancement in Cl(-). The changes are attributed to exchange of Na(+) for Ca(2+) in silicate ... Other/Unknown Material North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science Indian Pacific ENVELOPE(88.718000,-7.974800,57.496000,-11.336800) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
11-102 12-116 12-119 14-137 15-147 15-149 22-214 22-216 22-217 6-50 6-51 6-55 7-66 8-70 8-71 Caribbean Sea/BASIN Caribbean Sea/RIDGE Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Indian Ocean//RIDGE Leg11 Leg12 Leg14 Leg15 Leg22 Leg6 Leg7 Leg8 North Atlantic/BASIN North Atlantic/HILL North Atlantic/RIDGE North Atlantic/SEAMOUNT North Pacific/BASIN North Pacific/CONT RISE North Pacific/PLAIN North Pacific/RIDGE |
spellingShingle |
11-102 12-116 12-119 14-137 15-147 15-149 22-214 22-216 22-217 6-50 6-51 6-55 7-66 8-70 8-71 Caribbean Sea/BASIN Caribbean Sea/RIDGE Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Indian Ocean//RIDGE Leg11 Leg12 Leg14 Leg15 Leg22 Leg6 Leg7 Leg8 North Atlantic/BASIN North Atlantic/HILL North Atlantic/RIDGE North Atlantic/SEAMOUNT North Pacific/BASIN North Pacific/CONT RISE North Pacific/PLAIN North Pacific/RIDGE Sayles, Frederick L Manheim, Frank T Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
topic_facet |
11-102 12-116 12-119 14-137 15-147 15-149 22-214 22-216 22-217 6-50 6-51 6-55 7-66 8-70 8-71 Caribbean Sea/BASIN Caribbean Sea/RIDGE Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Indian Ocean//RIDGE Leg11 Leg12 Leg14 Leg15 Leg22 Leg6 Leg7 Leg8 North Atlantic/BASIN North Atlantic/HILL North Atlantic/RIDGE North Atlantic/SEAMOUNT North Pacific/BASIN North Pacific/CONT RISE North Pacific/PLAIN North Pacific/RIDGE |
description |
Through the Deep Sea Drilling Project samples of interstitial solutions of deeply buried marine sediments throughout the World Ocean have been obtained and analyzed. The studies have shown that in all but the most slowly deposited sediments pore fluids exhibit changes in composition upon burial. These changes can be grouped into a few consistent patterns that facilitate identification of the diagenetic reactions occurring in the sediments. Pelagic clays and slowly deposited (<1 cm/1000 yr) biogenic sediments are the only types that exhibit little evidence of reaction in the pore waters. In most biogenic sediments sea water undergoes considerable alteration. In sediments deposited at rates up to a few cm/1000 yr the changes chiefly involve gains of Ca(2+) and Sr(2+) and losses of Mg(2+) which balance the Ca(2+) enrichment. The Ca-Mg substitution may often reach 30 mM/kg while Sr(2+) may be enriched 15-fold over sea water. These changes reflect recrystallization of biogenic calcite and the substitution of Mg(2+) for Ca(2+) during this reaction. The Ca-Mg-carbonate formed is most likely a dolomitic phase. A related but more complex pattern is found in carbonate sediments deposited at somewhat greater rates. Ca(2+) and Sr(2+) enrichment is again characteristic, but Mg(2+) losses exceed Ca(2+) gains with the excess being balanced by SO4(post staggered 2-) losses. The data indicate that the reactions are similar to those noted above, except that the Ca(2+) released is not kept in solution but is precipitated by the HCO3(post staggered -) produced in SO4(post staggered 2-) reduction. In both these types of pore waters Na(+) is usually conservative, but K(+) depletions are frequent. In several partly consolidated sediment sections approaching igneous basement contact, very marked interstitial calcium enrichment has been found (to 5.5 g/kg). These phenomena are marked by pronounced depletion in Na(+), Si and CO2, and slight enhancement in Cl(-). The changes are attributed to exchange of Na(+) for Ca(2+) in silicate ... |
format |
Other/Unknown Material |
author |
Sayles, Frederick L Manheim, Frank T |
author_facet |
Sayles, Frederick L Manheim, Frank T |
author_sort |
Sayles, Frederick L |
title |
Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
title_short |
Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
title_full |
Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
title_fullStr |
Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
title_full_unstemmed |
Chemical composition of interstitial solutions from sediments of DSDP Legs 6-8, 11, 12, 14, 15, and 22 |
title_sort |
chemical composition of interstitial solutions from sediments of dsdp legs 6-8, 11, 12, 14, 15, and 22 |
publisher |
PANGAEA |
publishDate |
1975 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.706822 https://doi.org/10.1594/PANGAEA.706822 |
op_coverage |
MEDIAN LATITUDE: 18.161913 * MEDIAN LONGITUDE: -142.984900 * SOUTH-BOUND LATITUDE: -11.336800 * WEST-BOUND LONGITUDE: 88.718000 * NORTH-BOUND LATITUDE: 57.496000 * EAST-BOUND LONGITUDE: -7.974800 * DATE/TIME START: 1969-07-03T00:00:00 * DATE/TIME END: 1972-02-24T00:00:00 |
long_lat |
ENVELOPE(88.718000,-7.974800,57.496000,-11.336800) |
geographic |
Indian Pacific |
geographic_facet |
Indian Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Sayles, Frederick L; Manheim, Frank T (1975): Interstitial solutions and diagenesis in deeply buried marine sediments: results from the Deep Sea Drilling Project. Geochimica et Cosmochimica Acta, 39(2), 103-127, https://doi.org/10.1016/0016-7037(75)90165-9 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.706822 https://doi.org/10.1594/PANGAEA.706822 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.70682210.1016/0016-7037(75)90165-9 |
_version_ |
1809926931154468864 |