The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends

In addition to being of interest to ancient Greek and Roman historians, the site of Philippi, NE Greece, has long been noted in Quaternary circles for providing the longest continuous European pollen record, spanning the last one million years. Here the original age model is re-evaluated and a new m...

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Main Authors: Tzedakis, PC, Hooghiemstra, H, Palike, H
Format: Article in Journal/Newspaper
Language:unknown
Published: PERGAMON-ELSEVIER SCIENCE LTD 2006
Subjects:
Online Access:http://discovery.ucl.ac.uk/168183/
id ftucl:oai:eprints.ucl.ac.uk.OAI2:168183
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:168183 2023-05-15T16:39:18+02:00 The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends Tzedakis, PC Hooghiemstra, H Palike, H 2006-12 http://discovery.ucl.ac.uk/168183/ unknown PERGAMON-ELSEVIER SCIENCE LTD QUATERNARY SCI REV , 25 (23-24) 3416 - 3430. (2006) ISOTOPE SUBSTAGE 5E MIDDLE PLEISTOCENE CLIMATE VARIABILITY NORTHERN GREECE POLLEN RECORD DEEP SECTION ICE VOLUME SEA-LEVEL MARINE CORE Article 2006 ftucl 2016-01-21T23:21:44Z In addition to being of interest to ancient Greek and Roman historians, the site of Philippi, NE Greece, has long been noted in Quaternary circles for providing the longest continuous European pollen record, spanning the last one million years. Here the original age model is re-evaluated and a new marine-terrestrial correlation is proposed. An astronomical calibration procedure, based on a correspondence between changes in certain vegetation elements and March and June perihelion configurations, suggests that the base of the sequence extends back to 1.35 million years ago. The revised chronological framework for the Tenaghi Philippon sequence provides an opportunity to examine the long-term behaviour of individual taxa and vegetation trends within the context of global climate changes. Comparisons reveal a close correspondence between the terrestrial and marine records, in terms of orbital and suborbital variability. However, joint time-frequency analysis of the arboreal pollen record shows that the obliquity and eccentricity/precession signals persist into the '100-kyr' and '41-kyr' worlds, respectively, suggesting the operation of additional climate mechanisms that are independent of high-latitude glacial-interglacial effects. Unlike ice core and marine sequences, no change in the magnitude of interglacial tree population expansions is observed after the Mid-Brunhes Event. Instead, the Tenaghi Philippon record suggests a major shift in the vegetational composition of interglacials after MIS 16, with the establishment of forests of reduced diversity and a 'modern' appearance. (c) 2006 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper ice core University College London: UCL Discovery
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
topic ISOTOPE SUBSTAGE 5E
MIDDLE PLEISTOCENE
CLIMATE VARIABILITY
NORTHERN GREECE
POLLEN RECORD
DEEP SECTION
ICE VOLUME
SEA-LEVEL
MARINE
CORE
spellingShingle ISOTOPE SUBSTAGE 5E
MIDDLE PLEISTOCENE
CLIMATE VARIABILITY
NORTHERN GREECE
POLLEN RECORD
DEEP SECTION
ICE VOLUME
SEA-LEVEL
MARINE
CORE
Tzedakis, PC
Hooghiemstra, H
Palike, H
The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
topic_facet ISOTOPE SUBSTAGE 5E
MIDDLE PLEISTOCENE
CLIMATE VARIABILITY
NORTHERN GREECE
POLLEN RECORD
DEEP SECTION
ICE VOLUME
SEA-LEVEL
MARINE
CORE
description In addition to being of interest to ancient Greek and Roman historians, the site of Philippi, NE Greece, has long been noted in Quaternary circles for providing the longest continuous European pollen record, spanning the last one million years. Here the original age model is re-evaluated and a new marine-terrestrial correlation is proposed. An astronomical calibration procedure, based on a correspondence between changes in certain vegetation elements and March and June perihelion configurations, suggests that the base of the sequence extends back to 1.35 million years ago. The revised chronological framework for the Tenaghi Philippon sequence provides an opportunity to examine the long-term behaviour of individual taxa and vegetation trends within the context of global climate changes. Comparisons reveal a close correspondence between the terrestrial and marine records, in terms of orbital and suborbital variability. However, joint time-frequency analysis of the arboreal pollen record shows that the obliquity and eccentricity/precession signals persist into the '100-kyr' and '41-kyr' worlds, respectively, suggesting the operation of additional climate mechanisms that are independent of high-latitude glacial-interglacial effects. Unlike ice core and marine sequences, no change in the magnitude of interglacial tree population expansions is observed after the Mid-Brunhes Event. Instead, the Tenaghi Philippon record suggests a major shift in the vegetational composition of interglacials after MIS 16, with the establishment of forests of reduced diversity and a 'modern' appearance. (c) 2006 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Tzedakis, PC
Hooghiemstra, H
Palike, H
author_facet Tzedakis, PC
Hooghiemstra, H
Palike, H
author_sort Tzedakis, PC
title The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
title_short The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
title_full The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
title_fullStr The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
title_full_unstemmed The last 1.35 million years at Tenaghi Philippon: revised chronostratigraphy and long-term vegetation trends
title_sort last 1.35 million years at tenaghi philippon: revised chronostratigraphy and long-term vegetation trends
publisher PERGAMON-ELSEVIER SCIENCE LTD
publishDate 2006
url http://discovery.ucl.ac.uk/168183/
genre ice core
genre_facet ice core
op_source QUATERNARY SCI REV , 25 (23-24) 3416 - 3430. (2006)
_version_ 1766029631778979840