Loading…
New constraint on the maintenance of Mn nodules at the sediment surface
Investigations into the association of manganese nodules with pelagic sediment in many areas of the deep ocean have mainly considered either (1) the source of metals in nodules, or (2) the occurrence of nodules predominantly at the sediment surface. The second problem is duscussed here. The mechanis...
Saved in:
Published in: | Nature (London) 1980-08, Vol.286 (5776), p.880-883 |
---|---|
Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63 |
---|---|
cites | cdi_FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63 |
container_end_page | 883 |
container_issue | 5776 |
container_start_page | 880 |
container_title | Nature (London) |
container_volume | 286 |
creator | Piper, David Z. Fowler, Bradford |
description | Investigations into the association of manganese nodules with pelagic sediment in many areas of the deep ocean have mainly considered either (1) the source of metals in nodules, or (2) the occurrence of nodules predominantly at the sediment surface. The second problem is duscussed here. The mechanisms previously proposed have failed to consider that nodules retain their orientation at the sediment surface for several hundred-thousand years, during which time several tens of centimetres of sediment are fluxed down beneath them. Although we have no conclusive evidence, we consider the most plausible explanation for the surface occurrence of nodules to be bioturbation by infauna. |
doi_str_mv | 10.1038/286880a0 |
format | article |
fullrecord | <record><control><sourceid>crossref_sprin</sourceid><recordid>TN_cdi_crossref_primary_10_1038_286880a0</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>10_1038_286880a0</sourcerecordid><originalsourceid>FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63</originalsourceid><addsrcrecordid>eNpl0MFKxDAQBuAgCtZV8BFy1EN1kjTN9CiL7gqrXvRcYjLRLrupJC3i29t19eRpGPhm-PkZOxdwJUDhtcQaESwcsEJUpi6rGs0hKwAkloCqPmYnOa8BQAtTFWzxSJ_c9TEPyXZx4H3kwzvx7W6haKMj3gf-EHns_bihzO3wAzL5bkvTQR5TsI5O2VGwm0xnv3PGXu5un-fLcvW0uJ_frEorUQ4lkhHKBy-hwSmplLpRGpwlcj68emWUIYNYq8Zp7xuSRmstAnqqhGhsrWbsYv_XpT7nRKH9SN3Wpq9WQLsroP0rYKKXe5onEt8otet-THFK999-A1pHWi4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>New constraint on the maintenance of Mn nodules at the sediment surface</title><source>Nature</source><creator>Piper, David Z. ; Fowler, Bradford</creator><creatorcontrib>Piper, David Z. ; Fowler, Bradford</creatorcontrib><description>Investigations into the association of manganese nodules with pelagic sediment in many areas of the deep ocean have mainly considered either (1) the source of metals in nodules, or (2) the occurrence of nodules predominantly at the sediment surface. The second problem is duscussed here. The mechanisms previously proposed have failed to consider that nodules retain their orientation at the sediment surface for several hundred-thousand years, during which time several tens of centimetres of sediment are fluxed down beneath them. Although we have no conclusive evidence, we consider the most plausible explanation for the surface occurrence of nodules to be bioturbation by infauna.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/286880a0</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>Humanities and Social Sciences ; letter ; multidisciplinary ; Science ; Science (multidisciplinary)</subject><ispartof>Nature (London), 1980-08, Vol.286 (5776), p.880-883</ispartof><rights>Springer Nature Limited 1980</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63</citedby><cites>FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Piper, David Z.</creatorcontrib><creatorcontrib>Fowler, Bradford</creatorcontrib><title>New constraint on the maintenance of Mn nodules at the sediment surface</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>Investigations into the association of manganese nodules with pelagic sediment in many areas of the deep ocean have mainly considered either (1) the source of metals in nodules, or (2) the occurrence of nodules predominantly at the sediment surface. The second problem is duscussed here. The mechanisms previously proposed have failed to consider that nodules retain their orientation at the sediment surface for several hundred-thousand years, during which time several tens of centimetres of sediment are fluxed down beneath them. Although we have no conclusive evidence, we consider the most plausible explanation for the surface occurrence of nodules to be bioturbation by infauna.</description><subject>Humanities and Social Sciences</subject><subject>letter</subject><subject>multidisciplinary</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1980</creationdate><recordtype>article</recordtype><recordid>eNpl0MFKxDAQBuAgCtZV8BFy1EN1kjTN9CiL7gqrXvRcYjLRLrupJC3i29t19eRpGPhm-PkZOxdwJUDhtcQaESwcsEJUpi6rGs0hKwAkloCqPmYnOa8BQAtTFWzxSJ_c9TEPyXZx4H3kwzvx7W6haKMj3gf-EHns_bihzO3wAzL5bkvTQR5TsI5O2VGwm0xnv3PGXu5un-fLcvW0uJ_frEorUQ4lkhHKBy-hwSmplLpRGpwlcj68emWUIYNYq8Zp7xuSRmstAnqqhGhsrWbsYv_XpT7nRKH9SN3Wpq9WQLsroP0rYKKXe5onEt8otet-THFK999-A1pHWi4</recordid><startdate>19800828</startdate><enddate>19800828</enddate><creator>Piper, David Z.</creator><creator>Fowler, Bradford</creator><general>Nature Publishing Group UK</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19800828</creationdate><title>New constraint on the maintenance of Mn nodules at the sediment surface</title><author>Piper, David Z. ; Fowler, Bradford</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1980</creationdate><topic>Humanities and Social Sciences</topic><topic>letter</topic><topic>multidisciplinary</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Piper, David Z.</creatorcontrib><creatorcontrib>Fowler, Bradford</creatorcontrib><collection>CrossRef</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Piper, David Z.</au><au>Fowler, Bradford</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New constraint on the maintenance of Mn nodules at the sediment surface</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>1980-08-28</date><risdate>1980</risdate><volume>286</volume><issue>5776</issue><spage>880</spage><epage>883</epage><pages>880-883</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>Investigations into the association of manganese nodules with pelagic sediment in many areas of the deep ocean have mainly considered either (1) the source of metals in nodules, or (2) the occurrence of nodules predominantly at the sediment surface. The second problem is duscussed here. The mechanisms previously proposed have failed to consider that nodules retain their orientation at the sediment surface for several hundred-thousand years, during which time several tens of centimetres of sediment are fluxed down beneath them. Although we have no conclusive evidence, we consider the most plausible explanation for the surface occurrence of nodules to be bioturbation by infauna.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/286880a0</doi><tpages>4</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0028-0836 |
ispartof | Nature (London), 1980-08, Vol.286 (5776), p.880-883 |
issn | 0028-0836 1476-4687 |
language | eng |
recordid | cdi_crossref_primary_10_1038_286880a0 |
source | Nature |
subjects | Humanities and Social Sciences letter multidisciplinary Science Science (multidisciplinary) |
title | New constraint on the maintenance of Mn nodules at the sediment surface |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-18T11%3A40%3A55IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-crossref_sprin&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=New%20constraint%20on%20the%20maintenance%20of%20Mn%20nodules%20at%20the%20sediment%20surface&rft.jtitle=Nature%20(London)&rft.au=Piper,%20David%20Z.&rft.date=1980-08-28&rft.volume=286&rft.issue=5776&rft.spage=880&rft.epage=883&rft.pages=880-883&rft.issn=0028-0836&rft.eissn=1476-4687&rft_id=info:doi/10.1038/286880a0&rft_dat=%3Ccrossref_sprin%3E10_1038_286880a0%3C/crossref_sprin%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a282t-8e713dfd20982862259350caeecdfbd3737e788639c5dd9e275551f8de4119a63%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |