Loess distribution and related Quaternary sediments in the Carpathian Basin

被引:39
|
作者
Lehmkuhl, Frank [1 ]
Boesken, Janina [1 ]
Hosek, Jan [2 ]
Sprafke, Tobias [3 ]
Markovic, Slobodan B. [4 ]
Obreht, Igor [1 ,5 ,6 ]
Hambach, Ulrich [7 ,8 ]
Sumegi, Pal [9 ]
Thiemann, Arne [1 ]
Steffens, Stefanie [1 ]
Lindner, Heiko [1 ]
Veres, Daniel [10 ]
Zeeden, Christian [1 ,11 ]
机构
[1] Rhein Westfal TH Aachen, Dept Geog, Templergraben 55, D-52056 Aachen, Germany
[2] Czech Geol Survey, Prague, Czech Republic
[3] Univ Bern, Inst Geog, Bern, Switzerland
[4] Univ Novi Sad, Lab Paleoenvironm Reconstruct, Novi Sad, Serbia
[5] Univ Bremen, Organ Geochem Grp, MARUM Ctr Marine Environm Sci, Bremen, Germany
[6] Univ Bremen, Dept Geosci, Bremen, Germany
[7] Univ Bayreuth, BayCEER, Bayreuth, Germany
[8] Univ Bayreuth, Chair Geomorphol, Bayreuth, Germany
[9] Univ Szeged, Dept Geol & Palaeontol, Szeged, Hungary
[10] Romanian Acad, Inst Speol, Cluj Napoca, Romania
[11] PSL Res Univ, Observ Paris, IMCCE, Paris, France
来源
JOURNAL OF MAPS | 2018年 / 14卷 / 02期
关键词
Loess map; aeolian sediments; dust sources; spatial data; GIS; Pannonian Basin; palaeo-landscapes; SOUTHERN LIMIT; GLACIAL CYCLES; EUROPE; SERBIA; SEQUENCE; HUNGARY; SUTTO; MAP;
D O I
10.1080/17445647.2018.1526720
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
Supraregional (palaeo)geoecological studies require detailed knowledge of the distribution of aeolian sediments and their sources. Such spatial data can be visualised and shared in maps, but often these are constrained in their resolution or extent. This is the case for the Carpathian Basin, where cross-border maps are not detailed enough to answer many research questions. Problems occur especially along political borders due to different geological mapping standards and varying lithological definitions. Using a Geographic Information System (GIS), we compiled a map showing the distribution of loess and related Quaternary sediments in the Carpathian Basin, with unprecedented detail. We vectorised and analysed existing data (mainly from geological maps) and combined and transferred these into a common (loess) sediment classification system. This cross-border map shows the distribution of aeolian sediments in the Carpathian Basin at a scale of 1:1,500,000. For the northwestern and the southern Carpathian Basin, we added maps that clarify the extent of late Pleistocene and Holocene terrace and floodplain deposits, which were merged in the to highlight the predominant dust source areas for this region.
引用
收藏
页码:673 / 682
页数:10
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