COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN.
the Mediterranean area with the aim of reconstructing the Holocene climate changes. However, despite the fundamental progresses gained by the statistical analysis of compositional data (CODA), relatively few studies adopted an approach coherent with the fact that paleontological data are recorded as...
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ftunivnapoliiris:oai:www.iris.unina.it:11588/429117 2024-06-23T07:56:17+00:00 COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. DI DONATO, VALENTINO RUSSO ERMOLLI, ELDA Forlano S. Martín Fernández J. A. DI DONATO, Valentino Forlano, S. Martín Fernández, J. A. RUSSO ERMOLLI, Elda 2012 http://hdl.handle.net/11588/429117 eng eng Aiqua - THE TRANSITION FROM NATURAL TO ANTHROPOGENIC-DOMINATED ENVIRONMENTAL CHANGE IN ITALY AND THE SURROUNDING REGIONS SINCE THE NEOLITHIC http://hdl.handle.net/11588/429117 foraminifera holocene compositional data analysis 2012 ftunivnapoliiris 2024-06-10T14:58:48Z the Mediterranean area with the aim of reconstructing the Holocene climate changes. However, despite the fundamental progresses gained by the statistical analysis of compositional data (CODA), relatively few studies adopted an approach coherent with the fact that paleontological data are recorded as closed data (Buccianti and Esposito, 2004; Di Donato et al., 2008; 2009; Di Donato and Martín-Fernández, 2008). The planktonic foraminifera of G93-C9 core, recovered in the central Tyrrhenian Sea, were analyzed in order to reconstruct Holocene paleoclimatic changes in this sector of the Mediterranean. The foraminiferal record was analyzed by means of CODA, with the main aim of reconstructing the changes occurred during the mid-Holocene. Several studies indicate that from the mid-Holocene to the present the Mediterranean region has been characterized by drier condition and the establishement of the present-day Mediterranean climate (Jalut et al., 2000, Davis et al., 2003), however there is still debate on the anthropical contribution to such changes (i.a. Roberts et al., 2011). The reconstructions obtained from CODA of the G93-C9 core were compared with continental records of the western Mediterranean area in order to evaluate if changes in the marine and continental environment occurred simultaneously. Other/Unknown Material Planktonic foraminifera IRIS Università degli Studi di Napoli Federico II |
institution |
Open Polar |
collection |
IRIS Università degli Studi di Napoli Federico II |
op_collection_id |
ftunivnapoliiris |
language |
English |
topic |
foraminifera holocene compositional data analysis |
spellingShingle |
foraminifera holocene compositional data analysis DI DONATO, VALENTINO RUSSO ERMOLLI, ELDA Forlano S. Martín Fernández J. A. COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
topic_facet |
foraminifera holocene compositional data analysis |
description |
the Mediterranean area with the aim of reconstructing the Holocene climate changes. However, despite the fundamental progresses gained by the statistical analysis of compositional data (CODA), relatively few studies adopted an approach coherent with the fact that paleontological data are recorded as closed data (Buccianti and Esposito, 2004; Di Donato et al., 2008; 2009; Di Donato and Martín-Fernández, 2008). The planktonic foraminifera of G93-C9 core, recovered in the central Tyrrhenian Sea, were analyzed in order to reconstruct Holocene paleoclimatic changes in this sector of the Mediterranean. The foraminiferal record was analyzed by means of CODA, with the main aim of reconstructing the changes occurred during the mid-Holocene. Several studies indicate that from the mid-Holocene to the present the Mediterranean region has been characterized by drier condition and the establishement of the present-day Mediterranean climate (Jalut et al., 2000, Davis et al., 2003), however there is still debate on the anthropical contribution to such changes (i.a. Roberts et al., 2011). The reconstructions obtained from CODA of the G93-C9 core were compared with continental records of the western Mediterranean area in order to evaluate if changes in the marine and continental environment occurred simultaneously. |
author2 |
DI DONATO, Valentino Forlano, S. Martín Fernández, J. A. RUSSO ERMOLLI, Elda |
author |
DI DONATO, VALENTINO RUSSO ERMOLLI, ELDA Forlano S. Martín Fernández J. A. |
author_facet |
DI DONATO, VALENTINO RUSSO ERMOLLI, ELDA Forlano S. Martín Fernández J. A. |
author_sort |
DI DONATO, VALENTINO |
title |
COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
title_short |
COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
title_full |
COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
title_fullStr |
COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
title_full_unstemmed |
COMPOSITIONAL ANALYSIS OF PLANKTIC FORAMINIFERA AS A TOOL FOR THE INVESTIGATION OFMIDDLE TO LATE HOLOCENE CLIMATE CHANGES IN THE WESTERN MEDITERRANEAN. |
title_sort |
compositional analysis of planktic foraminifera as a tool for the investigation ofmiddle to late holocene climate changes in the western mediterranean. |
publishDate |
2012 |
url |
http://hdl.handle.net/11588/429117 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
Aiqua - THE TRANSITION FROM NATURAL TO ANTHROPOGENIC-DOMINATED ENVIRONMENTAL CHANGE IN ITALY AND THE SURROUNDING REGIONS SINCE THE NEOLITHIC http://hdl.handle.net/11588/429117 |
_version_ |
1802649270691561472 |