Climatostratigraphy of interglacials in Poland: Middle and Upper Pleistocene lower boundaries from a Polish perspective

Lindner, Leszek; Marks, Leszek; Nita, Małgorzata

doi:10.1016/j.quaint.2012.11.018

Cited by 65 publications

(40 citation statements)

References 13 publications

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“…It should be emphasised that views on the stratigraphic position of this succession are varied and have changed much over recent years. The most recent reports (Lindner & Marks 2015, Lindner et al 2013) situate the Augustovian and Domuratovian successions in the Podlasian interglacial between the Nidanian and Sanian 1 glaciations (Table 2).…”

Section: Discussionmentioning

confidence: 99%

Environmental and climate changes reflected in the Domuraty 2 section (NE Poland) based on analysis of plant macroremains

Stachowicz‐Rybka¹

2015

Acta Palaeobotanica

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ABSTRACT. Research in the Domuraty 2 section was focused on a series of lacustrine-river-swamp deposits in which the full spectrum of vegetation and climate changes was recognised in a detailed analysis of plant macroremains and a comparison with the results of pollen analysis. Based on plant macrofossil data, two (Dom II, Dom III) of three palynologically documented warm units were distinguished in the Domuraty succession. The palaeobotanical data from the Domuraty succession document several successive local vegetation changes in both interglacial and glacial periods, which can be related to global climate oscillations. The succession of local vegetation stands and changes in the vegetation, climate, water level, and trophy during the period of the Domuraty succession were analysed and compared with corresponding parameters of the Augustovian and Ferdynandovian interglacials. The taxonomically most diverse unit is Warm unit Dom II, with the highest share of taxa with high thermal requirements, which was compared to the older Augustovian (A II) and younger Ferdynandovian (F II) units. The comparison of the Domuratovian interglacial flora to that of the Korchevian interglacial in Belarus shows high similarity; most of the extinct taxa or taxa unknown in the present-day flora are common to the Korchevian and Domuratovian floras, suggesting similar age for these two communities. However, the Domuratovian flora lacks a few species important to the Korchevian flora, such as Stratiotes goretskyi, Carex rostrata-pliocenica, Brasenia sp., Caulinia antiqua, Aldrovanda borysthenica, and A. zusii.

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Section: Discussionmentioning

confidence: 99%

Environmental and climate changes reflected in the Domuraty 2 section (NE Poland) based on analysis of plant macroremains

Stachowicz‐Rybka¹

2015

Acta Palaeobotanica

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“…In the strati graphic schemes of both Po land and West ern Eu rope, this inter gla cial is at trib uted to MIS 15 (older tem per ate stage) and MIS 13 (youn ger one) in the Cromerian Com plex (Zagwijn, 1998;Lindner et al, 2013; Ta ble 1). At £uków, the esti mated tem per a ture range for pine for ests is from -12 to +15°C, and for steppe veg e ta tion from -17°C and -10 to +15°C (Pidek and Poska, 2013).…”

Section: Marine Records Of the Early Saalianmentioning

confidence: 99%

“…The se quence from £uków (Pidek and Poska, 2013), which is the sec ond in ter est ing pol len re cord re ported from the nearby site, re vealed a very com plex suc ces sion with the two-phased Ferdinandovian Inter gla cial and a se ries of neigh bour ing stadials and interstadials. It has been usu ally cor re lated with MIS 15 (lower tem per ate part) and MIS 13 (up per one) or gen er ally lo cated in the up per seg ments of the Cromerian Com plex (see Lindner et al, 2013). Hav ing high-res o lu tion pol len pro files at our dis posal, we test the pos si bil ity of cor re lat ing the ma rine re cords from the North At lan tic, es pe cially d 18 O of plank tic/ben thic fora mini fera and alkenone-based (U 37 k ¢ ) tem per a ture re con struc tions with pol len se quences on land.…”

Section: Introductionmentioning

confidence: 99%

Terrestrial versus marine archives: biostratigraphical correlation of the Middle Pleistocene lacustrine records from central Europe and their equivalents in the deep-sea cores from the Portuguese margin

Bińka

Marks

2018

Self Cite

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The palaeolake from Ossówka, east ern Po land, is an un usual ex am ple of ba sin, in which sed i men ta tion lasted from the begin ning of the Holsteinian through sev eral cli ma tic os cil la tions un til the Early Saalian, i.e. over a pe riod of ~70,000 years. This pro vides us with the op por tu nity of cor re lat ing the dy nam i cally chang ing events on land with their po ten tial equiv a lents in the ma rine pro files. Alkenone-based tem per a ture re con struc tions us ing U 37 k ¢ are an un usual tool in this re spect. Nev er theless, as a re sult, we suc cess fully re late this pol len se quence to the chang ing SST (sea sur face tem per a ture) val ues in the colder phases of MIS 11. The bi par tite Ferdinandovian Inter gla cial was pre vi ously cor re lated with the up per part of the Cromerian com plex (MIS 13 and MIS 15). Hav ing at our dis posal lim its in the SST alkenone-based re cord, we clearly iden tify the strati graphic po si tion of the sec ond warm phase of MIS 15 and a small frag ment of MIS 14. In our opin ion, the Rhume Inter gla cial, iden ti fied in Ger many, should be lo cated within MIS 13. Us ing the avail able or bit ally tuned chro nol ogy, we also give a sub stan tial in put to es ti mate du ra tion of these ter res trial interglacials, in di cat ing the start ing and end ing points of their equiv a lents in the alkenone re cords.

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“…Figure 1 shows the location of the Brasenia fossil finds, with records of different ages indicated with different symbols. The names of the Pleistocene stages were used by West (1968), Zagwijn (1996), Kondratiene (1996), Ber (2006), Lindner and Marks (2008), Molodkov and Bolikhovskaya (2010), Lindner et al (2013), as well as Yakubovskaya et al (2014). Correlation of these stages in different countries of Europe is given in Table 2.…”

Section: Pleistocene Fossils Of Brasenia In Europementioning

confidence: 99%

On the history of Brasenia Schreb. in the European Pleistocene

Drzymulska

2017

Veget Hist Archaeobot

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Climatostratigraphy of interglacials in Poland: Middle and Upper Pleistocene lower boundaries from a Polish perspective

Cited by 65 publications

References 13 publications

Environmental and climate changes reflected in the Domuraty 2 section (NE Poland) based on analysis of plant macroremains

Environmental and climate changes reflected in the Domuraty 2 section (NE Poland) based on analysis of plant macroremains

Terrestrial versus marine archives: biostratigraphical correlation of the Middle Pleistocene lacustrine records from central Europe and their equivalents in the deep-sea cores from the Portuguese margin

On the history of Brasenia Schreb. in the European Pleistocene

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