Krzysztof Ninard
Biographic Data
| ID | 5600747 |
|---|---|
| NAME | Krzysztof Ninard |
| GIVEN NAMES | Krzysztof |
| FAMILY NAME | Ninard |
| SIGNATURE | NINARD K |
| AFFILIATIONS | Jagiellonian University |
| ORCID | 0000-0002-7260-5979 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 6 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2022 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 1 |
Radiocarbon dates from deposits sampled at the Vistula Spit canal excavation (Southern Baltic coast, Poland)
We report new AMS radiocarbon dates of 16 samples from the Holocene deposits of the Vistula Spit, a large coastal barrier landform on the Southern Baltic coast. Collection of the samples was conducted directly from the sedimentary succession excavated during 2020–2022 construction of the Vistula Spit shipping canal. The dated material represents several paleosol horizons and peat lenses buried in the dune deposits, as well as their substrate – be…
Buried Podzols as a pedostratigraphic marker for the Medieval Climatic Optimum
The paleopedological record documented in aeolian dunes of the eastern European Sand Belt comprises predominantly Arenosols and only occasionally well-developed Podzols. There are several Late Pleistocene pedostratigraphic marker horizons of varied soil types designated in the European dune and loess deposits, but none falls within the range of the Holocene. Buried Podzol occurrences found recently in 10 inland dune sites dispersed throughout Cen…
New Radiocarbon Dates From Polish Inland Dunes Point to Prevalence of Human Impact on Dune Mobility
The timeframes of Holocene anthropogenic dune remobilization in Central Europe remain less studied compared to those of Late Glacial climatically controlled dune formation. The present contribution aims to reinforce existing knowledge on the chronology of Late Glacial–Holocene dune activity and stability, as well as to reveal the scale of human impact on dune remobilization. Accelerator mass spectrometry radiocarbon (AMS 14 C) dating and calibrat…
Holocene insect pioneer colonization of post-glacial dune sands exemplified by tiger beetle burrows
Many ecosystems today in temperate zones are the result of colonization of barren substrates deposited or exposed as a result of deglaciation, around the start of the Holocene. Direct evidence of post-glacial colonization, in the form of life traces such as tracks and burrows, is typically rare and erased by later succession unless buried deeply within a short time interval, as is possible in dune sands. Tiger beetles (Coleoptera: Cicindelidae) a…
Mammal tracks record anthropogenic environmental influence in late-Holocene inland dunes of the European Sand Belt, Poland
Structures previously suggested to be footprints or tracks, but which have been little described, were observed within Quaternary inland dunes of the European Sand Belt. Excavation of these in several localities of the eastern part of the belt in Poland reveal that they are hoofprints of various ungulate mammals, both wild and domestic, as well as footprints of humans, ranging from potentially as early as the fifth to sixth century to the 19th ce…
Mammal tracks record anthropogenic environmental influence in late-Holocene inland dunes of the European Sand Belt, Poland
Structures previously suggested to be footprints or tracks, but which have been little described, were observed within Quaternary inland dunes of the European Sand Belt. Excavation of these in several localities of the eastern part of the belt in Poland reveal that they are hoofprints of various ungulate mammals, both wild and domestic, as well as footprints of humans, ranging from potentially as early as the fifth to sixth century to the 19th ce…
Buried Podzols as a pedostratigraphic marker for the Medieval Climatic Optimum
The paleopedological record documented in aeolian dunes of the eastern European Sand Belt comprises predominantly Arenosols and only occasionally well-developed Podzols. There are several Late Pleistocene pedostratigraphic marker horizons of varied soil types designated in the European dune and loess deposits, but none falls within the range of the Holocene. Buried Podzol occurrences found recently in 10 inland dune sites dispersed throughout Cen…
New Radiocarbon Dates From Polish Inland Dunes Point to Prevalence of Human Impact on Dune Mobility
The timeframes of Holocene anthropogenic dune remobilization in Central Europe remain less studied compared to those of Late Glacial climatically controlled dune formation. The present contribution aims to reinforce existing knowledge on the chronology of Late Glacial–Holocene dune activity and stability, as well as to reveal the scale of human impact on dune remobilization. Accelerator mass spectrometry radiocarbon (AMS 14 C) dating and calibrat…
Holocene insect pioneer colonization of post-glacial dune sands exemplified by tiger beetle burrows
Many ecosystems today in temperate zones are the result of colonization of barren substrates deposited or exposed as a result of deglaciation, around the start of the Holocene. Direct evidence of post-glacial colonization, in the form of life traces such as tracks and burrows, is typically rare and erased by later succession unless buried deeply within a short time interval, as is possible in dune sands. Tiger beetles (Coleoptera: Cicindelidae) a…
Mammal tracks record anthropogenic environmental influence in late-Holocene inland dunes of the European Sand Belt, Poland
Structures previously suggested to be footprints or tracks, but which have been little described, were observed within Quaternary inland dunes of the European Sand Belt. Excavation of these in several localities of the eastern part of the belt in Poland reveal that they are hoofprints of various ungulate mammals, both wild and domestic, as well as footprints of humans, ranging from potentially as early as the fifth to sixth century to the 19th ce…
Buried Podzols as a pedostratigraphic marker for the Medieval Climatic Optimum
The paleopedological record documented in aeolian dunes of the eastern European Sand Belt comprises predominantly Arenosols and only occasionally well-developed Podzols. There are several Late Pleistocene pedostratigraphic marker horizons of varied soil types designated in the European dune and loess deposits, but none falls within the range of the Holocene. Buried Podzol occurrences found recently in 10 inland dune sites dispersed throughout Cen…
New Radiocarbon Dates From Polish Inland Dunes Point to Prevalence of Human Impact on Dune Mobility
The timeframes of Holocene anthropogenic dune remobilization in Central Europe remain less studied compared to those of Late Glacial climatically controlled dune formation. The present contribution aims to reinforce existing knowledge on the chronology of Late Glacial–Holocene dune activity and stability, as well as to reveal the scale of human impact on dune remobilization. Accelerator mass spectrometry radiocarbon (AMS 14 C) dating and calibrat…
Radiocarbon dates from deposits sampled at the Vistula Spit canal excavation (Southern Baltic coast, Poland)
We report new AMS radiocarbon dates of 16 samples from the Holocene deposits of the Vistula Spit, a large coastal barrier landform on the Southern Baltic coast. Collection of the samples was conducted directly from the sedimentary succession excavated during 2020–2022 construction of the Vistula Spit shipping canal. The dated material represents several paleosol horizons and peat lenses buried in the dune deposits, as well as their substrate – be…
Holocene (5 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Paleontology (4 works) · Paleosol (4 works) · Archaeology (3 works) · Geography (3 works) · Loess (3 works) · Physical geography (3 works) · Aeolian processes (2 works)