The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle–Late Pleistocene (MIS 6 – MIS 5). Radiocarbon‐dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of ~41–32 ka cal bp (Hengelo – Denekamp Interstadials). Holocene organic layers have also been found, with ¹⁴C ages within a range of 4330–4280 cal bp (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial.

中文翻译：

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GorzówWielkopolski（西北波兰）含Stephanorhinus kirchbergensis的第四纪古湖泊的地质，地层和古环境演化

GorzówWielkopolski地区暴露的沉积层序包括Eemian冰川间（MIS 5e）或Weichselian早期（MIS 5d–e）沉积物。沉积序列一直是广泛的跨学科研究的对象，这导致至少两个古湖层位的确定。两者都产生了大型哺乳动物的化石遗迹，以及花粉和植物大型化石。所有这些代理人已被用来重建沉积时普遍存在的环境条件，以及确定动物的地质背景和生物年代学位置。GS3序列的冰川河流层的光学激发发光测年分别为123.6±10.1（在下古湖以下）和72.0±5。2 ka（上古湖之上）表明该地点是在中晚更新世（MIS 6 – MIS 5）期间形成的。湖有机质的放射性碳测年表明，在中冰期（MIS 3）年龄段中，有一个紧密的簇，范围在〜41–32 ka calbp（Hengelo – Denekamp Interstadials）。还发现了全新世的有机层，其¹⁴ C年龄在4330–4280 cal bp范围内 （新石器时代）。花粉和植物的大化石记录，再加上沉积学和地球化学数据，证实了其到Eemian Interglacial的年代。