This fossil flora in Turkey stems from at least six Pliocene deposits in Güvem and Beşkonak villages, 80 kilometres (50 mi) north of Ankara, 22 kilometres (14 mi) north of Kızılcahamam and 125 kilometres (78 mi) south of the Black Sea coast. They are 1,000 metres (3,300 ft) to 1,500 metres (4,900 ft) above sea level, extending 15 kilometres (9.3 mi) north-south and 7 kilometres (4.3 mi) east-west. Between six and seven million years ago, a fresh water lake existed there in a forested area with mostly broad leaved deciduous tree species, dominated by sequoia and oak.

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Fossil flora of Kızılcahamam district
Stratigraphic range: Pliocene PreꞒ Ꞓ O S D C P T J K Pg N ↓
Location
Coordinates	40.61°N 32.68°E / 40.61; 32.68
Region	Kızılcahamam District, Ankara Province
Country	Turkey
Fossil flora of Kızılcahamam district (Turkey)

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This article may be confusing or unclear to readers. (June 2017)

The Turkish botany Professor Baki Kasaplıgil (1918-1992) from Çankırı who worked at the Biology Department, Mills College, Oakland, California from 1956 to 1992, made fossil collecting trips to the area around Kızılcahamam - Çerkeş road in 1964 and 1968. In the 1964 trip he collected fossil leaves of Glyptostrobus, Sequoia, Zelkova, Fagus, Carpinus, Ulmus, Quercus, Tilia and Acer. In the 1968 trip, he collected 400 plant parts such as leaves, seeds, fruits, twigs and branches. He also collected 50 fossils of frog and fish skeletons and larvae and insects. In 1969, Wayne Fry from University of Berkeley made plant fossil collections in Güvem. Daniel I. Axelrod also assisted in the research of this flora.^{[1][2][3][4][5]}

• Leaf fossils of Glyptostrobus europaeus (left) and Quercus drymeya (right) from the Pliocene of Kizilcahamam, found near Belpınar village by Osman Güldemir, a teacher at the Anadolu University in Eskişehir, Turkey.
• Güvem village with the Seyhamamı mosque.
• Columnar basalt formed by lava flows at Beşkonak village.
• Due to drying and cooling of the climate at the onset of the Pleistocene ice age in Kizilcahamam, the Sequoia forests with their many exotic plant species disappeared and have now been replaced by Scots pine (Pinus sylvestris) forests.
• Professor Baki Kasaplıgil collected many of his fossil specimens along dirt roads that had newly been made by a bulldozer.

• Sequoia, giant redwood forests were common at higher altitudes of Anatolia in the Tertiary and early Pleistocene.
• Sequoia
• Sequoia
• Sequoia branch of seed cones.
• Sequoia
• Sequoia
• Glyptostrobus europaeus may have survived in some refugia pockets of wetlands along Turkey's Black Sea coast until the early Holocene. Fossil Glyptostrobus europaeus pollen from early Holocene deposits prove such a recent existence of this species in Turkey. So recent fossil pollen have not been found in other countries bordering the Black Sea.
• Glyptostrobus
• Pinus canariensis
• Pinus canariensis
• Pinus canariensis
• Menispermum dauricum leaves
• Menispermum dauricum foliage
• Castanopsis
• Castanopsis
• Castanopsis acorns.
• Castanopsis
• Ailanthus
• Ailanthus seeds
• Comptonia
• Comptonia
• Comptonia
• Platycarya
• Platycarya
• Platycarya
• Astronium
• Magnolia sprengeri
• Magnolia sprengeri