...Figure 1. Multiproxy data from Tenaghi Philippon core TP-2005 (northeast Greece) and alignment with insolation. A: TP-2005 loss-on-ignition as percentage dry weight: organic matter, mass loss between 105 °C and 550 °C (solid line); carbonate content, mass loss between 550 °C and 950 °C (dashed...

... circulation in the North Atlantic. Model simulations and available proxy data suggest that it was strongest in the high to middle latitudes around the North Atlantic. Based on new pollen data from Tenaghi Philippon, northeastern Greece, we provide evidence for a massive climate-induced turnover in terrestrial...

... of events for this interval, while at the same time land sea correlations have been established. In Greece, hith- erto, two long pollen sequences covered the last climatic cycle, Tenaghi Philippon, eastern Macedonia (41)10*N, 24)20*E; 40 m above sea level (a.s.l (Wijmstra 1969; Wijmstra & Smit 1976...

... of the changes is beyond the resolution of any geochronological tool that can be currently applied to unlaminated lake sediments of MIS 3 age. The I-284 pollen record is here compared with two other Greek sequences from distinct local environmental settings: Tenaghi Philippon TF II, northeast Greece (41...

...Figure 1. Map of Greece showing the position of Mount Tymphi and the long Quaternary stratigraphical sequences of Tenaghi Philippon and Ioannina. ...

...) of the core Tenaghi Philippon II, Middle Pleistocene of Macedonia, Greece . Review of Palaeobotany and Palynology , 52 , 73 – 88 . Van der Weil A.M. Wijmstra T.A. 1987 b . Palynology of the 112.8–197.8 m interval of the core Tenaghi Philippon II, Middle Pleistocene of Macedonia...

... in developing a LCPR. This explains why the development and publication of the 587-m deep composite Funza09 record took some 40 years. Another famous pollen record is Tenaghi Philippon from Greece. This core was drilled in 1963 (upper 78 m) by the Geological Institute in Leiden. In 1977, shortly after Van...

... temperatures. However, other terrestrial sequences spanning the MBE have also suggested that pre-MBE interglacials were warmer than present day. This phenomenon has been well documented in the terrestrial record of Britain ( Candy et al., 2010 ) and in the long pollen record of Tenaghi Philippon (Greece...

...—Tenaghi Philippon; Zr—Zgierz-Rudunik; Zy—Żyardów. The tentative correlation of marine and terrestrial records shows ( Fig. 1 ) that the principal shifts of European environments were associated with SST changes in the North Atlantic. The marine IRD and N. pachyderma (sinistral) records...

...–Stari Slankamen sequence (number 3) and the Mircea Voda sequence (number 10). Locations of long Greek peat sequences Ioannina and Tenaghi Philippon are identified with numbers 15 and 16, respectively. We investigate the Late to Middle Pleistocene climate evolution (last 700 k.y.) of the southeast...

..., as evidenced by pollen records, is based mainly on lake cores from the Ioannina basin in northwest Greece and from Tenaghi Philippon in Macedonia. The latter contain high percentages of Artemisia pollen ( Wijmstra and Smit, 1976 ; Wijmstra et al., 1990 ; Mommersteeg et al., 1995 ), which...

... in the central Mediterranean region at Ioannina ( Tzedakis 1994 ) and Tenaghi Philippon ( Wijmstra 1969 ) in Greece, Valle di Castiglione ( Follieri et al. 1988 ) and Lago Grande di Monticchio ( Brauer et al. 2007 ) in Italy and Lake Orhid, Albania ( Lezine et al. 2010 ) that span the Last Interglacial–Last...

... Mountains were characterized by rapid and high-amplitude climate change. Indeed, suborbital frequencies have been noted in the relative pollen abundance of forest and open vegetation communities at Tenaghi Philippon in NE Greece for the last 450 ka ( Tzedakis et al . 2003 ). The sedimentological record...

... reported in the sediments of the Ionian Sea ( Keller et al., 1978 ) and has been traced across the Mediterranean ( Fig. 1A ; Item DR1 Table S1 in the GSA Data Repository 1 ). A precise age of 28,690–29,420 cal. yr B.P. was obtained for the Y-3 in the Tenaghi Philippon peat sequence, Greece ( Albert et al...

... climate covering a complete interglacial-glacial cycle and the Holocene are not available for the Gulf of Corinth specifically, because no deep cores have been collected. However, elsewhere in Greece, there are records that do span the last interglacial-glacial cycle (e.g., Ioannina, Kopais, Tenaghi...

... fjords [ 69 ]. A longer pollen record from Greece (Tenaghi Philippon) shows great fluctuations in vegetation communities and appearance of steppe vegetation in Southern Europe during not only substage 5d but also substages 7d and 9d [ 70 , 71 ]. Cryogenic deformations in the roof of the Kazantsevo...