Palaeotemperature estimation in the Holsteinian Interglacial (MIS 11) based on oxygen isotopes of aquatic gastropods from eastern Poland

Szymanek, Marcin

doi:10.1515/agp-2017-0023

Cited by 3 publications

(6 citation statements)

References 62 publications

(217 reference statements)

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“…8). However, previous studies from this site based on the oxygen isotopes of aquatic gastropods (Szymanek 2017) did not indicate significant differences between average water temperatures estimated for the Taxus and Pinus‐Larix zones. This data disagreement might be caused by the fact that molluscs' isotopic record reflects the growth‐season period, which rather points to stable conditions in the summer season.…”

Section: Discussionmentioning

confidence: 54%

“…Study site location with the hypothetical range of Ortel Królewski II palaeolake based on Szymanek (2017). …”

Section: Study Sitementioning

confidence: 99%

“…1995; Skompski 1996; Szymanek et al . 2005, 2016; Szymanek 2011, 2016, 2017, 2018). However, only low‐resolution malacological and ostracodological and pollen studies were conducted focused on the general changes of the faunal assemblage and its description through the whole sequence (Albrycht et al .…”

Section: Study Sitementioning

confidence: 99%

“…Former palynological, faunal, isotopic and geochemical studies have shown a great potential of this site for palaeoenvironmental studies of the Holsteinian interglacial (Albrycht et al 1995;Skompski 1996;Szymanek et al 2005Szymanek et al , 2016Szymanek 2011Szymanek , 2016Szymanek , 2017Szymanek , 2018. However, only low-resolution malacological and ostracodological and pollen studies were conducted focused on the general changes of the faunal assemblage and its description through the whole sequence (Albrycht et al 1995;Skompski 1996;Szymanek et al 2005;Szymanek 2011; Wasa z _ znik 2018).…”

Section: Study Sitementioning

confidence: 99%

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High‐resolution environmental changes recorded in ostracod and mollusc fauna from the Holsteinian palaeolake at Ortel Królewski II, eastern Poland

Czajkowska

2022

Boreas

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To better understand the environmental variability during the Holsteinian interglacial, fauna of the palaeolake deposits at Ortel Królewski II, eastern Poland was investigated. The analysis covered the uppermost part of the profile, representing the so‐called pre‐optimal part of the Holsteinian interglacial (MIS 11c), namely the Taxus and Pinus‐Larix pollen zones. Variability within the structure and composition of the faunal assemblage enabled a high‐resolution palaeoecological reconstruction – lake level and temperature fluctuations, its trophy and energy of the environment. During the Taxus pollen zone the lake was relatively deep and characterized by medium trophy conditions, which is indicated by a low abundance of molluscs of temporary water bodies and low numbers of Metacypris cordata and Scottia tumida. The temperature was rather stable with only small fluctuations during the transition between the Taxus and Pinus‐Larix zones. The occurrence of some cold‐loving ostracod species within the beginning of the Pinus‐Larix pollen zone indicates some deterioration of thermal conditions, which was additionally confirmed by using the mutual ostracod temperature range (MOTR) method. Lake level drop and expansion of reed zones within the Pinus‐Larix pollen zone are inferred from the increased abundance of shallow water ostracod and mollusc species as well as from an increased Bithynia‐index (BIN). The short cooling event documented early in the Pinus‐Larix zone in the studied profile might be an equivalent to the mid‐MIS 11c cooling, the so‐called Older Holsteinian Oscillation. Thus, the improved knowledge about the climate dynamics recorded within the sediments from this site contributes to a better understanding of the spatial extent and pattern of the climatic changes within the Holsteinian interglacial across Europe.

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Section: Discussionmentioning

confidence: 54%

“…Study site location with the hypothetical range of Ortel Królewski II palaeolake based on Szymanek (2017). …”

Section: Study Sitementioning

confidence: 99%

Section: Study Sitementioning

confidence: 99%

Section: Study Sitementioning

confidence: 99%

See 2 more Smart Citations

High‐resolution environmental changes recorded in ostracod and mollusc fauna from the Holsteinian palaeolake at Ortel Królewski II, eastern Poland

Czajkowska

2022

Boreas

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“…Ear lier iso to pic anal y sis from the Mazovian Inter gla cial (MIS 11c) fo cused on d 13 C (CaCO3) and d 18 O (CaCO3) of malacofauna shells (e.g., Nitychoruk, 2000;Szymanek et al, 2016;Szymanek, 2017). Ad di tion of d 13 C (org) al lows for ex tra in sight into palaeoenvironmental con di tions re corded by iso to pic com po sition of or ganic mat ter.…”

Section: Introductionmentioning

confidence: 99%

The rank of climatic oscillations during MIS 11c (OHO and YHO) and post-interglacial cooling during MIS 11b and MIS 11a in eastern Poland

Hrynowiecka

Żarski

Drzewicki

2019

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The rank of cli ma tic os cil la tions dur ing MIS 11c (OHO and YHO) and post-inter gla cial cool ing dur ing MIS 11b and MIS 11a in east ern Po land. Geo log i cal Quar terly, 63 (2): 375-394, doi: 10.7306/gq.1470 As so ci ate Ed i tor-Wojciech Granoszewski Lac us trine sed i ments rep re sent ing Ma rine Iso tope Stage 11 (MIS 11) were found in Hermanów (SE Po land) in a pres ent-day closed de pres sion un der a thin cover of Weichselian and Ho lo cene de pos its (1.4 m). These sed i ments filled a palaeolake cre ated as a re sult of melt ing of a dead-ice block at the end of MIS 12. Geo log i cal re search has ex cluded the pres ence of an ice sheet dur ing MIS 12 in this area. The lobe of the ice sheet of this gla ci ation was lo cated sev eral kilo metres to the west of Hermanów. The palaeolake was part of a larger palaeolakeland in south east ern Po land, formed dur ing MIS 11. The palaeomorphology of this inter gla cial is ev i dent in the con tem po rary re lief of the area and the out line of the lakes cor responds to the pat tern of the closed palaeodepressions. Based on the re cord of sed i ments from Hermanów, a new per spective re gard ing the sub-di vi sion of MIS 11 is pre sented. Two re gres sive phases are ob served in the Holsteinian Inter gla cial (MIS 11c)-OHO and YHO. The sub se quent substages with five cold fluc tu a tions ac cord ing to the new est strati graphic standards should be as signed to MIS 11b with a very clear cool ing and a slightly warmer MIS 11a. Car bon iso to pic com po si tion of or ganic mat ter cor rob o rates geo log i cal and en vi ron men tal anal y sis. The iso to pic com po si tion sug gests two cool ing pe ri ods: OHO and MIS 11b. Sta ble cli ma tic con di tions with lit tle tem per a ture fluc tu a tions per sisted be tween the cool ing pe ri ods. Key words: substages of MIS 11, Mazovian/Holsteinian Inter gla cial, MIS 12 and MIS 10 gla ci ation range, palaeoclimate changes, E Po land palaeolakeland, Car bon iso tope.

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Lacustrine molluscan carbonates: An interspecific approach toward the understanding of palaeoenvironmental conditions during the Holsteinian Interglacial (MIS 11) using δ18O and δ13C

Milano

Szymanek

2019

Palaeogeography, Palaeoclimatology, Palaeoecology

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Palaeotemperature estimation in the Holsteinian Interglacial (MIS 11) based on oxygen isotopes of aquatic gastropods from eastern Poland

Cited by 3 publications

References 62 publications

High‐resolution environmental changes recorded in ostracod and mollusc fauna from the Holsteinian palaeolake at Ortel Królewski II, eastern Poland

High‐resolution environmental changes recorded in ostracod and mollusc fauna from the Holsteinian palaeolake at Ortel Królewski II, eastern Poland

The rank of climatic oscillations during MIS 11c (OHO and YHO) and post-interglacial cooling during MIS 11b and MIS 11a in eastern Poland

Lacustrine molluscan carbonates: An interspecific approach toward the understanding of palaeoenvironmental conditions during the Holsteinian Interglacial (MIS 11) using δ18O and δ13C

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