Late Holocene environmental changes in the vicinity of Kültepe (Kayseri), Central Anatolia, Turkey

Şenkul, Çetin; ÖREN, Aziz; Doǧan, Uǧur; Eastwood, Warren J.

doi:10.1016/j.quaint.2017.12.044

Cited by 12 publications

(9 citation statements)

References 25 publications

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“…According to the fossil pollen data obtained from different locations in Anatolia, between 5000-3200 BP in Southwest Anatolia (Figure 1; Bakker et al, 2012;Bakker et al, 2013;Bottema and Woldring, 1984;Eastwood et al, 1999;Roberts, 1990;Vermoere et al, 2000) and North Anatolia (Bottema and Woldring, 1990;Bottema et al, 1993Bottema et al, -1994Ocakoğlu et al, 2016), between 4000-3200 BP in Western Anatolia (Müllenhoff et al, 2004) and Northwest Anatolia (Leroy et al, 2002;Miebach et al, 2016), in Central Anatolia between 4800-1650 BP (Ören, 2018;Şenkul et al, 2018;Turner et al, 2008) and in Eastern Anatolia between 4000-3000 BP (Biltekin et al, 2018;Landmann et al, 1996;van Zeist and Woldring, 1978;Wick et al, 2003), it is seen that natural forest vegetation was dominant before the beginning of the intensive agriculture period. In this period, while woody pollen rates are high in pollen diagrams, herbaceous pollen rates are low.…”

Section: Period In Which Natural Vegetation Is Conservedmentioning

confidence: 98%

“…The lack of studies evaluating the pollen changes and their characteristic features used in the interpretation of fossil pollen diagrams and determining the periods of palaeovegetation and palaeoland use in a field made this study necessary. For this purpose, in this study, in the light of the results of the fossil pollen analysis studies carried out in Southwest Anatolia (Bakker et al, 2012;Bottema and Woldring, 1984;Eastwood et al, 1998;Kaniewski et al, 2007;Vermoere et al, 2002), North Anatolia (Bottema et al, 1993(Bottema et al, -1994Izdebski, 2013;Leroy et al, 2010), Northwest Anatolia (Leroy et al, 2002;Miebach et al, 2016), Western Anatolia (Müllenhoff et al, 2004;Sullivan, 1988), Central Anatolia (Eastwood et al, 2009;England et al, 2008;Ören, 2018;Roberts et al, 2016;Şenkul et al, 2018) and Eastern Anatolia (Biltekin et al, 2018;Eriş et al, 2018) covering the years 5000-1000 BP, the periods of palaeoland use that emerged with human influence and the characteristics of the palaeovegetation changes that took place in these periods are given together.…”

Section: Introductionmentioning

confidence: 99%

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Fosil Polen Kayıtlarına Göre Orta-Geç Holosen’de Anadolu’da Arazi Kullanımı ve Vejetasyonda Meydana Gelen Değişimler

ÖREN

2022

Coğrafi Bilimler Dergisi

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Paleovejetasyon değişimleri ve paleoarazi kullanımı özelliklerinin belirlenmesinde en önemli veriler fosil polen kayıtları ve bu kayıtlar içerisinde yer alan antropojenik göstergelerdir. Bu çalışmada fosil polen kayıtlarından elde edilen diyagramlardaki göstergeler değerlendirilerek paleoarazi kullanım dönemleri ve paleovejetasyon değişimlerinin belirlenmesi ve paleocoğrafya araştırmacılarının kullanımına sunulması amaçlanmıştır. Bu amaç doğrultusunda Anadolu'da farklı lokasyonlarda gerçekleştirilen fosil polen çalışmaları değerlendirilmiş ve üç farklı dönem belirlenmiştir; 1. Doğal vejetasyonun korunduğu dönemde yüksek rekabet yeteneğine sahip ağaç polenleri görülmüştür. 2. Orman tahribi ve yoğun tarım döneminde doğal ormanın tahribatı sonucunda istilacı vejetasyon gelişimini gösteren bitkilere ait polen taksonları ve antropojenik göstergeler yayılış göstermiştir. 3.Arazinin geçici olarak terk edilme döneminde antropojenik göstergeler ile ormanların tahrip edildiği sahalarda yayılış gösteren bitkiler belirgin şekilde azalırken, ikincil ormanların gelişimi görülmüştür.

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Section: Period In Which Natural Vegetation Is Conservedmentioning

confidence: 98%

Section: Introductionmentioning

confidence: 99%

Fosil Polen Kayıtlarına Göre Orta-Geç Holosen’de Anadolu’da Arazi Kullanımı ve Vejetasyonda Meydana Gelen Değişimler

ÖREN

2022

Coğrafi Bilimler Dergisi

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“…Given the nature and scale of impact in Australia has been so great in such a relatively short time, the impacts in areas such as Central Anatolia must have been equally or even more severe. Central Anatolia has a long history of agricultural impact, that includes periods of abundance and famine, aridity, erosion, deforestation and reforestation, and abandonment and recolonization [37,38] . Periods of warmer and drier climate have had devastating effects and are considered to have been driven by global processes [37] .…”

Section: Ecological Status Of Semi-arid Cropping Areasmentioning

confidence: 99%

A Case for Assessing Allocasuarina and Casuarina Spp. For Use in Agroecosystem Improvement in Semi-Arid Areas With a Focus on Central Anatolia, Turkey

Riley¹

2021

Front. Agr. Sci. Eng.

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Agroecosystems in water-limited contexts-Mediterranean, semi-arid and arid climatic zones-are too frequently degraded systems that will not provide the needed ecosystem services to ensure a future of sustainable agricultural production. The processes that have created this situation continue and are being accelerated by anthropogenic climate change. Increasing arboreal vegetation in these areas through agroforestry is an important strategy to conserve and improve their agroecosystems. Actinorhizal trees and shrubs in the Casurinaceae have a unique set of adaptations for heat and water stress, and/or infertile to hostile soils. Central Anatolia, Turkey is particularly at risk of increasing aridity and further degradation. Therefore, species of Allocasuarina and Casuarina have been evaluated for their potential use in agroecosystem improvement in semi-arid areas with a focus on Central Anatolia. Based on a semiquantitative environmental tolerance index and reported plant stature, eight species were identified as being of high (A. verticillata and C. pauper) to moderate (A. acutivalvis, A. decaisneana, A. dielsiana, A. huegeliana, C. cristata and C. obesa) priority for assessment, with none of these species having been adequately evaluated for agroforestry deployment in semi-arid agroecosystems in any context.

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“…In fossil pollen studies, this period showing the effect of humans on vegetation in mid-to late-Holocene is called the Beyşehir Occupation Phase (BOP) (Bottema and Woldring, 1984;Eastwood et al, 1998). Castanea, Fraxinus ornus, Olea europaea, Juglans, Vitis, Plantago lanceolata and Sanguisorba taxa, observed in the pollen diagrams of many fossil pollen studies in Southwestern Anatolia and Central Anatolia, are evidence of the BOP (England, 2006;England et al 2008;Şenkul, 2018). The effect of BOP on the pollen diagram of Lake Tuzla is seen between 3230 BP and 1115 BP.…”

Section: Accepted Manuscriptmentioning

confidence: 99%

Mid-to late-Holocene paleovegetation change in vicinity of Lake Tuzla (Kayseri), Central Anatolia, Turkey

Şenkul

Memiş

Eastwood

et al. 2018

Quaternary International

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Late Holocene environmental changes in the vicinity of Kültepe (Kayseri), Central Anatolia, Turkey

Cited by 12 publications

References 25 publications

Fosil Polen Kayıtlarına Göre Orta-Geç Holosen’de Anadolu’da Arazi Kullanımı ve Vejetasyonda Meydana Gelen Değişimler

Fosil Polen Kayıtlarına Göre Orta-Geç Holosen’de Anadolu’da Arazi Kullanımı ve Vejetasyonda Meydana Gelen Değişimler

A Case for Assessing Allocasuarina and Casuarina Spp. For Use in Agroecosystem Improvement in Semi-Arid Areas With a Focus on Central Anatolia, Turkey

Mid-to late-Holocene paleovegetation change in vicinity of Lake Tuzla (Kayseri), Central Anatolia, Turkey

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