20:
214:
375:
128:
1168:
Lundmark, Anders
Mattias; Lamminen, Jarkko (2016). "The provenance and setting of the Mesoproterozoic Dala Sandstone, western Sweden, and paleogeographic implications for southwestern Fennoscandia".
814:
Japsen, Peter; Green, Paul F.; Bonow, Johan M.; Erlström, Mikael (2016). "Episodic burial and exhumation of the southern Baltic Shield: Epeirogenic uplifts during and after break-up of
Pangaea".
147:
the peneplain tilts west and north respectively. This is reflected in that the southeastern part of the lake is very shallow but gets progressively deeper towards the northwest. In
528:; Bonow, Johan M.; Japsen, Peter (2013). "Stratigraphic Landscape Analysis and geomorphological paradigms: Scandinavia as an example of Phanerozoic uplift and subsidence".
179:
plateau in Norway is the Sub-Cambrian peneplain has been uplifted at least thousand meters, albeit
Hardangervidda itself is part of a much younger peneplain formed in the
1343:
280:
of the East
European Platform freed it in geologically recent times. Further southeast a series of burried inselbergs on top the peneplain have been identified through
1258:
Nielsen, Arne Thorshøj; Schovsbo, Niels
Hemmingsen (2011). "The Lower Cambrian of Scandinavia: Depositional environment, sequence stratigraphy and palaeogeography".
322:. The basement rocks forming the peneplain surface were exhumed from depths where the temperature was in excess of 100 °C prior to the formation of peneplain.
970:"Automatic identification of topographic surfaces related to the sub-Cambrian peneplain (SCP) in southern Norway—Surface generation algorithms and implications"
88:
The Sub-Cambrian peneplain extends as an almost continuous belt along the eastern coast of Sweden for some 700 km from north to south. Near
Stockholm and
729:
61:
parts of this peneplain are extraordinarily flat with relief of less than 20 m. The overlying cover rocks demonstrate that the peneplain was flooded by
342:. Sheet wash would also have hindered the formation of deep weathering profiles. Indeed, at the places the substrate of the Sub-Cambrian peneplain is
416:
have likely never been recycled. This means the parent rocks of the sandstone were eroded and the sediment strongly reworked and weathered reaching
1137:"A large array of inselbergs on a continuation of the sub-Cambrian peneplain in the Baltic Basin: evidence from seismic data, Western Lithuania"
851:
Plains, steps, hilly relief and valleys in northern Sweden – review, interpretations and implications for conclusions on
Phanerozoic tectonics
65:
during the Early
Paleozoic. Being the oldest identifiable peneplain in its area the Sub-Cambrian peneplain qualifies as a primary peneplain.
404:
in changing configurations. The new relief formed on top of
Cambrian sediments smoothed out irregularities in the peneplain. Early Cambrian
116:
and to the east in eastern Småland. At this last region the sub-Cambrian peneplain is truncated to the west by a well defined and prominent
100:
where it is dissected by joint valleys. The Sub-Cambrian peneplain in the crestal region of the South
Swedish Dome is the highest step in a
1292:"Provenance and sedimentary processes controlling the formation of lower Cambrian quartz arenite along the southwestern margin of Baltica"
1909:
669:"The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield"
96:
is the Sub-Cambrian peneplain is both highly uplifted and eroded. More inland the peneplain can be traced at the crestal region of the
1777:
724:
308:
peneplain from this period has been preserved. The low relief terrain on which the Jotnian sandstone deposited was disturbed by the
1329:
1077:
1858:
421:
1336:
1045:
1468:
1443:
1418:
1296:
725:"Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins"
1237:
1041:
911:
Hall, Adrian M.; Krabbendam, Maarten; van Boeckel, Mikis; Hättestrand, Clas; Ebert, Karin; Heyman, Jakob (2019-12-01).
1919:
857:
530:
913:
The sub-Cambrian unconformity in Västergötland, Sweden: Reference surface for Pleistocene glacial erosion of basement
1904:
1833:
1787:
1581:
1393:
939:
Lidmar-Bergström, Karna (1993). "Denudation surfaces and tectonics in the southernmost part of the Baltic Shield".
121:
1894:
1807:
1561:
1290:
Lorentzen, Sanne; Augustsson, Carita; Nystuen, Johan P.; Bernd, Jasper; Jahren, Jens; Schovsbo, Niels H. (2018).
1103:
883:
879:
846:
777:
720:
626:
562:
525:
323:
312:
in western Sweden about 1,000 million years ago and then begun to erode again into a terrain of subdued relief.
77:
108:. In southern Sweden the peneplain surfaces tilt away from the crest of South Swedish Dome, to the northwest in
1889:
1843:
417:
1914:
1738:
1683:
1403:
1398:
974:
782:
631:
397:
319:
140:
97:
143:
the peneplain extends further west being 450 km wide from west to east. Immediately east and south of lake
1853:
1792:
1728:
599:
425:
392:
laterally close to the exhumed parts of the peneplain and also close to the buried parts of the peneplain.
309:
237:
168:
1868:
1812:
1748:
1260:
420:
with no other in-between step or hiatus. The source areas for these sandstones are local rocks from the
281:
241:
152:
1233:"Ediacaran to early Cambrian weathering of the Kautokeino Greenstone Belt in Finnmark, northern Norway"
187:
1002:
252:
sediments that rests above much of the peneplain. The peneplain is characterized by a general lack of
1848:
1586:
1494:
1170:
1112:
1050:
941:
888:
496:
401:
305:
1733:
1576:
19:
1828:
1509:
1388:
567:
229:
1652:
1556:
1232:
199:
109:
1899:
1528:
1203:
1022:
690:
339:
62:
1657:
1622:
1107:
1003:"Mountains of southernmost Norway: uplifted Miocene peneplains and re-exposed Mesozoic surfaces"
113:
1617:
1546:
816:
594:
385:
363:
338:
is thought to have been an important process of erosion leading to the formation of extensive
269:
156:
1802:
1713:
1305:
1269:
1212:
1179:
1148:
1014:
983:
950:
825:
791:
738:
682:
640:
608:
576:
539:
454:
327:
1231:
Bjørlykke, Arne; Rueslåtten, Håkon; Van der Lelij, Roelant; Schønenberger, Jasmin (2022).
232:
is a continuation of the peneplain. To the east the Sub-Cambrian peneplain continues as an
1863:
1688:
1463:
1217:
1198:
668:
429:
301:
191:
172:
101:
1772:
1566:
1458:
748:
257:
217:
69:
213:
1642:
1607:
1571:
1551:
1383:
1373:
912:
203:
176:
164:
132:
968:
Jarsve, Erlend M.; Krøgli, Svein Olav; Etzelmüller, Bernd; Gabrielsen, Roy H. (2014).
850:
1883:
1838:
1797:
1627:
1612:
1499:
1478:
1453:
1448:
1378:
1368:
1352:
1291:
1026:
954:
795:
694:
673:
644:
449:
335:
1273:
1183:
543:
23:
Extraordinary flat surfaces of the Sub-Cambrian peneplain around the shores of Lake
1763:
1360:
987:
580:
444:
374:
233:
127:
76:
publishing the first extensive map in 1954. This mapping has been improved upon by
73:
50:
1001:
Japsen, Peter; Green, Paul F.; Chalmers, James A.; Bonow, Johan M. (17 May 2018).
686:
597:; Finkl Jr., Charles W. (1980). "Cratonic erosion unconformities and peneplains".
1309:
1782:
1723:
1698:
1647:
1637:
1473:
474:
265:
249:
148:
1136:
1743:
1693:
1538:
1514:
1408:
261:
117:
105:
93:
89:
28:
1197:
Bingen, Bernard; Andersson, Jenny; Söderlund, Ulf; Möller, Charlotte (2008).
829:
1662:
743:
405:
378:
351:
331:
285:
273:
253:
221:
195:
54:
39:
1667:
167:
in Norway have been interpreted to be part of the peneplain that has been
144:
24:
1321:
1246:
413:
389:
355:
347:
316:
245:
135:
plateau in the Norway is believed to be an uplifted part of the peneplain
43:
1018:
330:
with a preceding brief valley phase and that it grades down to a former
1708:
1703:
1632:
1504:
1435:
1135:
Grendaitė, Milda; Michelevičius, Dainius; Radzevičius, Sigitas (2022).
499:
432:
297:
277:
240:. On a grand-scale the peneplain is not completely flat as it has been
207:
180:
160:
58:
1718:
1602:
409:
359:
343:
300:
imply that much of the Baltic Shield have had faint relief since the
53:. Eastward, where this peneplain dips below Cambrian and other Lower
46:
1153:
969:
780:(1995). "Relief and saprolites through time on the Baltic Shield".
612:
565:(1988). "Denudation surfaces of a shield area in southern Sweden".
373:
315:
The peneplain formed after 600 million years ago but prior to the
212:
126:
18:
400:
very large areas were swiftly flooded forming large and shallow
381:
1325:
92:
the peneplain is densely dissected by joint valleys and at the
667:
Lidmar-Bergström, Karna; Olvmo, Mats; Bonow, Johan M. (2017).
486:
This is known from borehole explorations and seismic profiles.
723:; Japsen, Peter; Bonow, Johan M.; Chalmers, James A. (2013).
396:
The flatness of the peneplain meant that during the Cambrian
334:. Due to the absence of land vegetation in Precambrian times
841:
839:
520:
518:
155:, there is some uncertainty over whether the hilltops are
42:) that has been exhumed and exposed by erosion from under
629:(1996). "Long term morphotectonic evolution in Sweden".
276:
after its formation. Blå Jungfrun remained buried until
350:
the peneplain is roughly coeval with the formation of
1076:
Amantov, Aleksey; Feldskaar, Willy (March 26, 2015).
918:(Report). Swedish Nuclear Fuel and Wast Management Co
326:
and co-workers assume the peneplain formed through a
190:
in northern Sweden the peneplain occur, as result of
346:
it never exceeds a few meters in depth. In Norway's
1821:
1761:
1676:
1595:
1536:
1527:
1487:
1434:
1427:
1359:
1071:
1069:
730:
Geological Survey of Denmark and Greenland Bulletin
495:There have been suggestions of the existence of an
194:, at about 650 meters giving origin to a series of
224:and island formed in connection to the peneplain.
1285:
1283:
809:
807:
805:
171:and is apparently disrupted by NNE-SSW trending
38:is an ancient, extremely flat, erosion surface (
714:
712:
710:
708:
706:
704:
502:peneplain. This has, however, not been proved.
366:with marine sedimentary rock of Cambrian age.
1337:
1199:"The Mesoproterozoic in the Nordic countries"
8:
934:
932:
772:
770:
768:
766:
408:overlying the peneplain in southern Norway,
662:
660:
658:
656:
654:
557:
555:
553:
1533:
1431:
1344:
1330:
1322:
1216:
1152:
742:
264:which is an ancient inselberg formed in
159:. A similar situation occurs in central
16:Ancient, extremely flat, erosion surface
1078:"Det subkambriske peneplanet i Baltika"
514:
466:
1247:https://dx.doi.org/10.17850/njg102-3-1
1046:"Finland: Terrängformer och berggrund"
256:. One exception to this is the island
7:
68:The surface was first identified by
473:The scarp can be observed east of
14:
1116:(in Swedish). Cydonia Development
1054:(in Swedish). Cydonia Development
1007:Journal of the Geological Society
892:(in Swedish). Cydonia Development
1778:Central Skåne Volcanic Province
1274:10.1016/j.earscirev.2010.12.004
1218:10.18814/epiiugs/2008/v31i1/005
1184:10.1016/j.precamres.2016.01.003
544:10.1016/j.gloplacha.2012.10.015
362:up to 15 m below the surface's
1859:Transscandinavian Igneous Belt
988:10.1016/j.geomorph.2013.12.032
581:10.1080/04353676.1988.11880265
422:Transscandinavian Igneous Belt
1:
687:10.1080/11035897.2017.1364293
163:. Further west, parts of the
151:, at the northern end of the
1310:10.1016/j.sedgeo.2017.08.008
1238:Norwegian Journal of Geology
955:10.1016/0301-9268(93)90086-H
796:10.1016/0169-555X(94)00076-4
645:10.1016/0169-555X(95)00083-H
228:In northwestern Finland the
72:in a 1910 publication, with
858:Geological Survey of Sweden
531:Global and Planetary Change
248:to erosion and the load of
120:that separates it from the
1936:
1910:Geology of European Russia
1834:Blekinge-Bornholm Province
1788:Kattsund-Koster dyke swarm
1444:Billingen terminal moraine
1582:Sorgenfrei-Tornquist Zone
1562:Nordfjord-Sogn Detachment
1419:Sub-Mesozoic hilly relief
244:. This deformation is an
157:remnants of the peneplain
1844:Scandinavian Caledonides
1587:South Finland Shear Zone
1505:Jotnian sedimentary rock
830:10.1016/j.gr.2015.06.005
627:Lidmar-Bergströrm, Karna
175:. Near the 1,100 m high
1854:Sveconorwegian Province
1684:Central Swedish lowland
1469:Skövde terminal moraine
1394:South Småland peneplain
1353:Geology of Fennoscandia
1104:Lidmar-Bergström, Karna
880:Lidmar-Bergström, Karna
847:Lidmar-Bergström, Karna
778:Lidmar-Bergström, Karna
744:10.34194/geusb.v30.4673
721:Lidmar-Bergström, Karna
526:Lidmar-Bergström, Karna
141:Central Swedish lowland
122:South Småland peneplain
1808:Särna Alkaline Complex
1793:Kola Alkaline Province
1729:Scandinavian Mountains
1414:Sub-Cambrian peneplain
884:"Sydsvenska höglandet"
849:; Olvmo, Mats (2015).
600:The Journal of Geology
393:
370:Sedimentary rock cover
324:Karna Lidmar-Bergström
310:Sveconorwegian orogeny
238:East European Platform
225:
136:
112:, to the northeast in
78:Karna Lidmar-Bergström
49:over large swathes of
36:sub-Cambrian peneplain
31:
1869:Western Gneiss Region
1849:Svecofennian Province
1822:Provinces and orogens
1813:Satakunta dyke swarms
1749:White Sea Rift System
1261:Earth-Science Reviews
595:Fairbridge, Rhodes W.
377:
216:
169:tectonically uplifted
130:
22:
1689:Gulf of Bothnia rift
1596:Large impact craters
1495:Alum Shale Formation
1171:Precambrian Research
1141:Geological Quarterly
1113:Nationalencyklopedin
1051:Nationalencyklopedin
942:Precambrian Research
889:Nationalencyklopedin
751:on 24 September 2015
418:sedimentary maturity
1829:Belomorian Province
1389:Ostrobothnian Plain
1297:Sedimentary Geology
1019:10.1144/jgs2017-157
568:Geografiska Annaler
296:Interpretations of
230:Ostrobothnian Plain
198:including those of
1920:Planation surfaces
1739:South Swedish Dome
1699:Lake Ladoga graben
1013:(5): jgs2017–157.
394:
282:seismic reflection
246:isostatic response
226:
153:Swedish West Coast
137:
98:South Swedish Dome
32:
1905:Erosion landforms
1877:
1876:
1803:Rapakivi granites
1757:
1756:
1694:Lake Inari graben
1618:Hummeln structure
1523:
1522:
1428:Sedimentary cover
1042:Lundqvist, Thomas
817:Gondwana Research
298:Jotnian sandstone
80:since the 1980s.
57:cover rocks. The
1927:
1895:Cambrian geology
1714:Norrland terrain
1534:
1510:Reusch's Moraine
1488:Sedimentary rock
1432:
1346:
1339:
1332:
1323:
1314:
1313:
1287:
1278:
1277:
1268:(3–4): 207–310.
1255:
1249:
1229:
1223:
1222:
1220:
1194:
1188:
1187:
1165:
1159:
1158:
1156:
1132:
1126:
1125:
1123:
1121:
1100:
1094:
1093:
1091:
1089:
1073:
1064:
1063:
1061:
1059:
1037:
1031:
1030:
998:
992:
991:
965:
959:
958:
949:(1–4): 337–345.
936:
927:
926:
924:
923:
917:
908:
902:
901:
899:
897:
876:
870:
869:
867:
865:
855:
843:
834:
833:
811:
800:
799:
774:
761:
760:
758:
756:
747:. Archived from
746:
719:Green, Paul F.;
716:
699:
698:
664:
649:
648:
623:
617:
616:
591:
585:
584:
563:Lidmar-Bergström
559:
548:
547:
522:
503:
493:
487:
484:
478:
471:
455:Norrland terrain
328:cycle of erosion
1935:
1934:
1930:
1929:
1928:
1926:
1925:
1924:
1890:Cambrian Europe
1880:
1879:
1878:
1873:
1864:Timanide Orogen
1817:
1753:
1677:Morphostrucures
1672:
1591:
1519:
1483:
1464:Sevetti moraine
1423:
1404:200 m peneplain
1399:300 m peneplain
1355:
1350:
1319:
1317:
1289:
1288:
1281:
1257:
1256:
1252:
1230:
1226:
1196:
1195:
1191:
1167:
1166:
1162:
1154:10.7306/gq.1633
1134:
1133:
1129:
1119:
1117:
1102:
1101:
1097:
1087:
1085:
1082:geoforskning.no
1075:
1074:
1067:
1057:
1055:
1040:Behrens, Sven;
1039:
1038:
1034:
1000:
999:
995:
967:
966:
962:
938:
937:
930:
921:
919:
915:
910:
909:
905:
895:
893:
878:
877:
873:
863:
861:
853:
845:
844:
837:
813:
812:
803:
776:
775:
764:
754:
752:
718:
717:
702:
666:
665:
652:
625:
624:
620:
593:
592:
588:
561:
560:
551:
524:
523:
516:
512:
507:
506:
494:
490:
485:
481:
472:
468:
463:
441:
372:
302:Mesoproterozoic
294:
192:tectonic uplift
188:Stöttingfjället
104:system seen in
102:piedmonttreppen
86:
17:
12:
11:
5:
1933:
1931:
1923:
1922:
1917:
1915:Unconformities
1912:
1907:
1902:
1897:
1892:
1882:
1881:
1875:
1874:
1872:
1871:
1866:
1861:
1856:
1851:
1846:
1841:
1836:
1831:
1825:
1823:
1819:
1818:
1816:
1815:
1810:
1805:
1800:
1795:
1790:
1785:
1780:
1775:
1769:
1767:
1759:
1758:
1755:
1754:
1752:
1751:
1746:
1744:Vättern graben
1741:
1736:
1734:Scanian horsts
1731:
1726:
1721:
1716:
1711:
1706:
1701:
1696:
1691:
1686:
1680:
1678:
1674:
1673:
1671:
1670:
1665:
1660:
1655:
1650:
1645:
1643:Ritland crater
1640:
1635:
1630:
1625:
1620:
1615:
1610:
1608:Gardnos crater
1605:
1599:
1597:
1593:
1592:
1590:
1589:
1584:
1579:
1577:Röjnoret Fault
1574:
1572:Protogine Zone
1569:
1564:
1559:
1554:
1552:Iapetus Suture
1549:
1547:Burträsk Fault
1543:
1541:
1531:
1525:
1524:
1521:
1520:
1518:
1517:
1515:Visingsö Group
1512:
1507:
1502:
1497:
1491:
1489:
1485:
1484:
1482:
1481:
1476:
1471:
1466:
1461:
1456:
1451:
1446:
1440:
1438:
1429:
1425:
1424:
1422:
1421:
1416:
1411:
1406:
1401:
1396:
1391:
1386:
1384:Paleic surface
1381:
1376:
1374:Hardangervidda
1371:
1365:
1363:
1357:
1356:
1351:
1349:
1348:
1341:
1334:
1326:
1316:
1315:
1279:
1250:
1224:
1189:
1160:
1127:
1095:
1084:(in Norwegian)
1065:
1032:
993:
960:
928:
903:
871:
835:
801:
762:
700:
681:(4): 244–259.
650:
618:
613:10.1086/628474
586:
575:(4): 337–350.
549:
513:
511:
508:
505:
504:
488:
479:
465:
464:
462:
459:
458:
457:
452:
447:
440:
437:
426:Sveconorwegian
386:Byrum's raukar
371:
368:
293:
290:
177:Hardangervidda
165:Paleic surface
133:Hardangervidda
124:to the west.
85:
82:
15:
13:
10:
9:
6:
4:
3:
2:
1932:
1921:
1918:
1916:
1913:
1911:
1908:
1906:
1903:
1901:
1898:
1896:
1893:
1891:
1888:
1887:
1885:
1870:
1867:
1865:
1862:
1860:
1857:
1855:
1852:
1850:
1847:
1845:
1842:
1840:
1839:Kola Province
1837:
1835:
1832:
1830:
1827:
1826:
1824:
1820:
1814:
1811:
1809:
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1704:Lofoten horst
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1613:Granby crater
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1500:Hedmark Group
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1479:Veiki moraine
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1454:Rogen moraine
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1379:Muddus plains
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1369:Borsu surface
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1361:Paleosurfaces
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450:Muddus plains
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398:transgression
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200:Ångermanälven
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110:Västergötland
107:
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71:
66:
64:
60:
56:
52:
48:
45:
41:
37:
30:
26:
21:
1773:Alnö Complex
1719:Omberg horst
1709:Muhos Graben
1658:Söderfjärden
1567:Pärvie Fault
1557:Lainio Fault
1459:Salpausselkä
1413:
1318:
1301:
1295:
1265:
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1242:
1236:
1227:
1211:(1): 29–34.
1208:
1202:
1192:
1175:
1169:
1163:
1144:
1140:
1130:
1118:. Retrieved
1111:
1098:
1086:. Retrieved
1081:
1058:November 30,
1056:. Retrieved
1049:
1035:
1010:
1006:
996:
979:
973:
963:
946:
940:
920:. Retrieved
906:
896:November 30,
894:. Retrieved
887:
874:
862:. Retrieved
860:. p. 12
821:
815:
787:
781:
753:. Retrieved
749:the original
734:
728:
678:
672:
636:
630:
621:
607:(1): 69–86.
604:
598:
589:
572:
566:
535:
529:
491:
482:
469:
445:Baltic Klint
395:
314:
295:
258:Blå Jungfrun
236:beneath the
234:unconformity
227:
218:Blå Jungfrun
185:
138:
131:Much of the
114:Östergötland
87:
74:Sten Rudberg
70:Arvid Högbom
67:
63:shallow seas
51:Fennoscandia
35:
33:
1783:Fen Complex
1724:Oslo Graben
1648:Siljan Ring
1539:shear zones
1537:Faults and
1474:Trollgarden
1304:: 203–217.
1178:: 197–208.
1108:"Inselberg"
824:: 357–377.
538:: 153–171.
500:Sub-Jotnian
402:inland seas
266:Precambrian
250:Phanerozoic
204:Indalsälven
1884:Categories
1798:Norra Kärr
1653:Sääksjärvi
1623:Lappajärvi
1529:Structures
1409:Strandflat
922:2020-11-26
856:(Report).
510:References
406:sandstones
344:kaolinized
336:sheet wash
262:Baltic Sea
254:inselbergs
196:water gaps
94:High Coast
90:Hudiksvall
29:Kinnekulle
1900:Ediacaran
1766:provinces
1663:Suvasvesi
1088:April 29,
1027:134575021
982:: 89–99.
790:: 45–61.
695:134300755
639:: 33–59.
379:Limestone
352:kaolinite
340:pediments
332:sea level
304:, but no
286:Lithuania
274:sandstone
268:time and
222:inselberg
55:Paleozoic
40:peneplain
1436:Moraines
1204:Episodes
1120:June 22,
864:June 29,
755:30 April
439:See also
414:Bornholm
356:smectite
348:Finnmark
317:Cambrian
242:deformed
149:Bohuslän
44:Cambrian
1764:igneous
1762:Lesser
1633:Lumparn
497:exhumed
433:orogens
430:Gothian
424:or the
364:contact
306:exhumed
278:erosion
260:in the
208:Ljusnan
183:epoch.
181:Miocene
161:Halland
139:In the
106:Småland
59:exposed
1668:Tvären
1603:Dellen
1025:
737:: 18.
693:
410:Scania
382:stacks
360:illite
292:Origin
270:buried
173:faults
145:Vänern
84:Extent
47:strata
25:Vänern
1147:(1).
1023:S2CID
916:(PDF)
854:(PDF)
691:S2CID
475:Växjö
461:Notes
390:Öland
220:, an
118:scarp
27:near
1638:Mien
1245:(3)
1122:2015
1090:2016
1060:2017
898:2017
866:2016
757:2015
573:70 A
428:and
412:and
358:and
206:and
34:The
1306:doi
1302:375
1270:doi
1266:107
1243:102
1213:doi
1180:doi
1176:275
1149:doi
1015:doi
1011:175
984:doi
980:211
951:doi
826:doi
792:doi
739:doi
683:doi
679:139
674:GFF
641:doi
609:doi
577:doi
540:doi
536:100
388:in
384:of
284:in
272:in
186:At
1886::
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1282:^
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1235:,
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1080:.
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1021:.
1009:.
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882:.
838:^
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804:^
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703:^
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953::
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794::
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643::
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611::
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542::
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