New palaeoclimate reconstructions based on multidisciplinary investigation in the Ferdynandów 2011 stratotype site (eastern Poland)

Stachowicz‐Rybka, Renata; Pidek, Irena Agnieszka; Żarski, Marcin

doi:10.7306/gq.1353

Cited by 2 publications

(4 citation statements)

References 16 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…During the Miocene and Pliocene, Pterocarya became common among European wetland vegetation (Mai 1995;Reumer and Wessels 2003). Fossil records indicate that Pterocarya was inferred to still have a large distribution throughout Europe by the Early Pleistocene (Hrynowiecka and Winter 2016;Segota1967;Stachowicz-Rybka et al 2017). Due to significant climate cooling from the end of the Miocene and especially the end of the Pliocene, a major ice sheet expansion occurred in Europe (Zachos et al 2001).…”

Section: Historic Expansion and Contraction: Integrating Fossil Records Enm And Phylogeographic Surveysmentioning

confidence: 99%

“…The role of Pterocarya become significant in the pollen floras of Neogene period (Miocene and Pliocene), thus indicating the common occurrence of the wingnut in the wetland vegetation of Europe in this epoch. During the Pleistocene, pollen grains of Pterocarya were found in NE, WE, CE and EE in all interglacial phases, until the Holsteinian (Binka et al 2003;Hrynowiecka and Winter 2016;Krupinski 1995;Nitychoruk 1994;Segota 1967;Stachowicz-Rybka et al 2017;Winter 2001). In Southern Europe, Pterocarya pollen was found in most profiles, ranging from very low frequencies, from less than 2% to even more than 50% in the Middle Pleistocene site of Riano (Follieri 1962), where also macroremains of wingnut were discovered (Follieri 1958).…”

Section: Fossil Record Synthesis Of Pterocarya In Europementioning

confidence: 99%

See 1 more Smart Citation

Past, present and future suitable areas for the relict tree Pterocarya fraxinifolia (Juglandaceae): Integrating fossil records, niche modeling, and phylogeography for conservation

et al. 2021

Self Cite

View full text Add to dashboard Cite

Pterocarya fraxinifolia, native to the southern Caucasus and adjacent areas, has been widely introduced in Europe. In this study, we investigate the following: (1) How did its current distribution form? (2) What are the past, current, and future suitable habitats of P. fraxinifolia? (3) What is the best conservation approach? Ecological niche modeling was applied to determine its climatic demands and project the distribution of climatically suitable areas during three periods of past, current, and future (2070) time. Then, an integrated analysis of fossil data was performed. Massive expansion of Pterocarya species between the Miocene and Pliocene facilitated the arrival of P. fraxinifolia to the southern Caucasus. The Last Glacial Maximum played a vital role in its current fragmented spatial distribution in the Euxinian and Hyrcanian regions with lower elevations, and Caucasian and Irano-Turanian regions with higher elevations. Climatic limiting factors were very different across these four regions. Future climate change will create conditions for the expansion of this species in Europe. Human activities significantly decreased the suitable area for P. fraxinifolia, especially in the Euxinian, Hyrcanian, and Irano-Turanian regions. Considering genetic diversity, climate vulnerability, and land utilization, the Euxinian, Hyrcanian, and Irano-Turanian regions have been recognized as conservation priority areas for P. fraxinifolia.

show abstract

Section: Historic Expansion and Contraction: Integrating Fossil Records Enm And Phylogeographic Surveysmentioning

confidence: 99%

Section: Fossil Record Synthesis Of Pterocarya In Europementioning

confidence: 99%

Past, present and future suitable areas for the relict tree Pterocarya fraxinifolia (Juglandaceae): Integrating fossil records, niche modeling, and phylogeography for conservation

et al. 2021

Self Cite

View full text Add to dashboard Cite

show abstract

“…2) was described by Pidek (2015), Stachowicz‐Rybka (2015c), Stachowicz‐Rybka et al . (2017) and Winter (2017). It contains successions covering two warm periods separated by a cooling stage.…”

Section: Study Sitesmentioning

confidence: 99%

“…During the second optimum (F2), these basins became shallow eutrophic lakes overgrown by Brasenia borysthenica , and at the end of this period transformed into peat bogs (Stachowicz‐Rybka et al . 2017). The presence of macrophytes was favourable for the roach, rudd and tench.…”

Section: Palaeoenvironmental Implicationsmentioning

confidence: 99%

Pleistocene freshwater environments of Poland: a comprehensive study of fish assemblages based on a multi‐proxy approach

Stefaniak

Kovalchuk

Kotusz

et al. 2020

Boreas

View full text Add to dashboard Cite

The results of a comprehensive study of Pleistocene fish‐bearing localities from the territory of Poland are presented. Fish remains came from lacustrine deposits and cave sites representing a time‐span from the late Early Pleistocene until the Early Holocene. Here we present the taxonomic composition and species diversity of all known fish assemblages from Poland. In total, 23 species belonging to 20 genera of eight families were identified. Cyprinids were the most taxonomically diverse, followed by salmonids and percids. Other families were each represented only by a single species. The roach, rudd, bream, pike and perch were the most common components of the Pleistocene fish assemblages of Poland. These assemblages are clearly divided into two groups representing palaeolakes and cave sites. A significant taxonomic similarity is observed between fish assemblages from Poland and those of Chibanian and Late Pleistocene ages from central and eastern Europe. Pleistocene environments and climates of Poland are characterized using a multi‐proxy approach (analysis of stable isotopes, plant macro‐remains, pollen, molluscs and cladocerans). Obtained data allowed us to estimate a number of parameters of Pleistocene water bodies of the Polish Lowland (reservoir type, trophism, oxygen content, depth and water level changes, bottom character, and flow speed). The formation of freshwater fish assemblages was influenced by dynamic changes in the hydrographic network, and climatic changes during the Pleistocene and Holocene. Their development was favoured by the formation of lakes after melting of the ice sheet.

show abstract

New palaeoclimate reconstructions based on multidisciplinary investigation in the Ferdynandów 2011 stratotype site (eastern Poland)

Cited by 2 publications

References 16 publications

Past, present and future suitable areas for the relict tree Pterocarya fraxinifolia (Juglandaceae): Integrating fossil records, niche modeling, and phylogeography for conservation

Past, present and future suitable areas for the relict tree Pterocarya fraxinifolia (Juglandaceae): Integrating fossil records, niche modeling, and phylogeography for conservation

Pleistocene freshwater environments of Poland: a comprehensive study of fish assemblages based on a multi‐proxy approach

Contact Info

Product

Resources

About