Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)
Identifieur interne : 001B70 ( Main/Merge ); précédent : 001B69; suivant : 001B71Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)
Auteurs : Meinrad KüttelSource :
- Boreas [ 0300-9483 ] ; 1977-10.
Abstract
New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.
Url:
DOI: 10.1111/j.1502-3885.1977.tb00293.x
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 001483
- to stream Istex, to step Curation: 001483
- to stream Istex, to step Checkpoint: 001677
Links to Exploration step
ISTEX:A612D176663A94A89609F0344F92E32AA6A51DE7Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><author><name sortKey="Kuttel, Meinrad" sort="Kuttel, Meinrad" uniqKey="Kuttel M" first="Meinrad" last="Küttel">Meinrad Küttel</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:A612D176663A94A89609F0344F92E32AA6A51DE7</idno><date when="1977" year="1977">1977</date><idno type="doi">10.1111/j.1502-3885.1977.tb00293.x</idno><idno type="url">https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001483</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001483</idno><idno type="wicri:Area/Istex/Curation">001483</idno><idno type="wicri:Area/Istex/Checkpoint">001677</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">001677</idno><idno type="wicri:doubleKey">0300-9483:1977:Kuttel M:pollenanalytische:und:geochronologische</idno><idno type="wicri:Area/Main/Merge">001B70</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><author><name sortKey="Kuttel, Meinrad" sort="Kuttel, Meinrad" uniqKey="Kuttel M" first="Meinrad" last="Küttel">Meinrad Küttel</name><affiliation><wicri:noCountry code="subField">1976</wicri:noCountry></affiliation></author></analytic><monogr></monogr><series><title level="j">Boreas</title><idno type="ISSN">0300-9483</idno><idno type="eISSN">1502-3885</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1977-10">1977-10</date><biblScope unit="volume">6</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="259">259</biblScope><biblScope unit="page" to="274">274</biblScope></imprint><idno type="ISSN">0300-9483</idno></series><idno type="istex">A612D176663A94A89609F0344F92E32AA6A51DE7</idno><idno type="DOI">10.1111/j.1502-3885.1977.tb00293.x</idno><idno type="ArticleID">BOR259</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0300-9483</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.</div></front></TEI></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Bois/explor/CheneBelgiqueV1/Data/Main/Merge
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001B70 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Main/Merge/biblio.hfd -nk 001B70 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Bois
|area= CheneBelgiqueV1
|flux= Main
|étape= Merge
|type= RBID
|clé= ISTEX:A612D176663A94A89609F0344F92E32AA6A51DE7
|texte= Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)
}}
| This area was generated with Dilib version V0.6.27. |  |