Class information for: |
Basic class information |
Class id | #P | Avg. number of references |
Database coverage of references |
---|---|---|---|
2638 | 3510 | 48.5 | 31% |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
Cluster id | Level | Cluster label | #P |
---|---|---|---|
4 | 4 | ENVIRONMENTAL SCIENCES//GEOSCIENCES, MULTIDISCIPLINARY//METEOROLOGY & ATMOSPHERIC SCIENCES | 1766162 |
31 | 3 | GEOGRAPHY, PHYSICAL//GEOSCIENCES, MULTIDISCIPLINARY//HOLOCENE | 107938 |
2638 | 2 | ARABIAN ARCHAEOLOGY AND EPIGRAPHY//DEAD SEA//ARCHAEOLOGY | 3510 |
10466 | 1 | AFRICAN HUMID PERIOD//LIMNOL UNIT//MARINE PALYNOLOGY | 1061 |
12618 | 1 | SAHARA//NUBIAN AQUIFER//CENTRAL SAHARA | 893 |
17381 | 1 | ARABIAN ARCHAEOLOGY AND EPIGRAPHY//ARABIA//PRE AKSUMITE | 602 |
19338 | 1 | DEAD SEA//LAKE LISAN//NEAR EASTERN STUDIES UNIT | 510 |
23951 | 1 | QANAT//NABATAEAN ARCHITECTURE//ANCIENT DESERT AGRICULTURE | 329 |
34146 | 1 | PARALIC ECOSYSTEMS//NORTHERNMOST CHILE//NADOR | 115 |
Terms with highest relevance score |
rank | Term | termType | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|---|
1 | ARABIAN ARCHAEOLOGY AND EPIGRAPHY | journal | 1174262 | 6% | 63% | 213 |
2 | DEAD SEA | authKW | 146894 | 2% | 26% | 65 |
3 | ARCHAEOLOGY | WoSSC | 129794 | 21% | 2% | 735 |
4 | AFRICAN HUMID PERIOD | authKW | 123798 | 1% | 65% | 22 |
5 | ARABIA | authKW | 114163 | 2% | 24% | 54 |
6 | SAHARA | authKW | 97839 | 2% | 21% | 54 |
7 | QANAT | authKW | 88048 | 1% | 56% | 18 |
8 | LAKE LISAN | authKW | 86459 | 0% | 76% | 13 |
9 | PRE AKSUMITE | authKW | 69581 | 0% | 100% | 8 |
10 | PALAEOECOLOGY OF AFRICA | journal | 67467 | 0% | 52% | 15 |
Web of Science journal categories |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | Archaeology | 129794 | 21% | 2% | 735 |
2 | Geography, Physical | 57038 | 22% | 1% | 756 |
3 | Geosciences, Multidisciplinary | 42557 | 41% | 0% | 1423 |
4 | Paleontology | 12851 | 8% | 1% | 292 |
5 | Anthropology | 8606 | 8% | 0% | 274 |
6 | Water Resources | 3483 | 9% | 0% | 316 |
7 | Asian Studies | 1802 | 2% | 0% | 57 |
8 | Geochemistry & Geophysics | 1352 | 6% | 0% | 214 |
9 | Limnology | 1350 | 3% | 0% | 88 |
10 | Geology | 1287 | 3% | 0% | 100 |
Address terms |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | LIMNOL UNIT | 61208 | 1% | 27% | 26 |
2 | TOURISM ARCHAEOL | 38965 | 0% | 41% | 11 |
3 | ARCHAEOL | 33952 | 5% | 2% | 171 |
4 | LARGE LAKES OBSERV | 32584 | 1% | 11% | 34 |
5 | DIPARTIMENTO SCI ANTICHITA | 28151 | 1% | 18% | 18 |
6 | DFG SH ING EARTHS SUR E VARIABLE ENVI | 27831 | 0% | 80% | 4 |
7 | DIPARTIMENTO STUDI RIC AFRICA PAESI ARABI | 27831 | 0% | 80% | 4 |
8 | GEOL PLICAT | 27831 | 0% | 80% | 4 |
9 | HUMAN ORIGINS PALAEOENVIRONM GRP | 27831 | 0% | 80% | 4 |
10 | IRAKL | 27831 | 0% | 80% | 4 |
Journals |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | ARABIAN ARCHAEOLOGY AND EPIGRAPHY | 1174262 | 6% | 63% | 213 |
2 | PALAEOECOLOGY OF AFRICA | 67467 | 0% | 52% | 15 |
3 | AFRICAN ARCHAEOLOGICAL REVIEW | 41533 | 1% | 17% | 28 |
4 | JOURNAL OF AFRICAN ARCHAEOLOGY | 37890 | 1% | 20% | 22 |
5 | QUATERNARY RESEARCH | 25680 | 3% | 3% | 89 |
6 | QUATERNARY SCIENCE REVIEWS | 25587 | 3% | 3% | 118 |
7 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY | 22414 | 4% | 2% | 141 |
8 | QUATERNARY INTERNATIONAL | 20464 | 3% | 2% | 112 |
9 | ANTHROPOLOGIE | 19436 | 1% | 5% | 47 |
10 | AZANIA-ARCHAEOLOGICAL RESEARCH IN AFRICA | 18755 | 1% | 12% | 18 |
Author Key Words |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
LCSH search | Wikipedia search |
---|---|---|---|---|---|---|---|
1 | DEAD SEA | 146894 | 2% | 26% | 65 | Search DEAD+SEA | Search DEAD+SEA |
2 | AFRICAN HUMID PERIOD | 123798 | 1% | 65% | 22 | Search AFRICAN+HUMID+PERIOD | Search AFRICAN+HUMID+PERIOD |
3 | ARABIA | 114163 | 2% | 24% | 54 | Search ARABIA | Search ARABIA |
4 | SAHARA | 97839 | 2% | 21% | 54 | Search SAHARA | Search SAHARA |
5 | QANAT | 88048 | 1% | 56% | 18 | Search QANAT | Search QANAT |
6 | LAKE LISAN | 86459 | 0% | 76% | 13 | Search LAKE+LISAN | Search LAKE+LISAN |
7 | PRE AKSUMITE | 69581 | 0% | 100% | 8 | Search PRE+AKSUMITE | Search PRE+AKSUMITE |
8 | HOLOCENE | 56941 | 5% | 3% | 190 | Search HOLOCENE | Search HOLOCENE |
9 | RUB AL KHALI | 52186 | 0% | 100% | 6 | Search RUB+AL+KHALI | Search RUB+AL+KHALI |
10 | CENTRAL SAHARA | 51155 | 0% | 59% | 10 | Search CENTRAL+SAHARA | Search CENTRAL+SAHARA |
Core articles |
The table includes core articles in the class. The following variables is taken into account for the relevance score of an article in a cluster c: (1) Number of references referring to publications in the class. (2) Share of total number of active references referring to publications in the class. (3) Age of the article. New articles get higher score than old articles. (4) Citation rate, normalized to year. |
Rank | Reference | # ref. in cl. |
Shr. of ref. in cl. |
Citations |
---|---|---|---|---|
1 | GATTO, M , ZERBONI, A , (2015) HOLOCENE SUPRA-REGIONAL ENVIRONMENTAL CHANGES AS TRIGGER FOR MAJOR SOCIO-CULTURAL PROCESSES IN NORTHEASTERN AFRICA AND THE SAHARA.AFRICAN ARCHAEOLOGICAL REVIEW. VOL. 32. ISSUE 2. P. 301 -333 | 68 | 75% | 3 |
2 | OSLISLY, R , WHITE, L , BENTALEB, I , FAVIER, C , FONTUGNE, M , GILLET, JF , SEBAG, D , (2013) CLIMATIC AND CULTURAL CHANGES IN THE WEST CONGO BASIN FORESTS OVER THE PAST 5000 YEARS.PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES. VOL. 368. ISSUE 1625. P. - | 38 | 95% | 13 |
3 | DRAKE, NA , BREEZE, P , PARKER, A , (2013) PALAEOCLIMATE IN THE SAHARAN AND ARABIAN DESERTS DURING THE MIDDLE PALAEOLITHIC AND THE POTENTIAL FOR HOMININ DISPERSALS.QUATERNARY INTERNATIONAL. VOL. 300. ISSUE . P. 48 -61 | 47 | 62% | 31 |
4 | BREEZE, PS , GROUCUTT, HS , DRAKE, NA , WHITE, TS , JENNINGS, RR , PETRAGLIA, MD , (2016) PALAEOHYDROLOGICAL CORRIDORS FOR HOMININ DISPERSALS IN THE MIDDLE EAST SIMILAR TO 250-70,000 YEARS AGO.QUATERNARY SCIENCE REVIEWS. VOL. 144. ISSUE . P. 155 -185 | 58 | 50% | 1 |
5 | AMARAL, PGC , VINCENS, A , GUIOT, J , BUCHET, G , DESCHAMPS, P , DOUMNANG, JC , SYLVESTRE, F , (2013) PALYNOLOGICAL EVIDENCE FOR GRADUAL VEGETATION AND CLIMATE CHANGES DURING THE AFRICAN HUMID PERIOD TERMINATION AT 13 DEGREES N FROM A MEGA-LAKE CHAD SEDIMENTARY SEQUENCE.CLIMATE OF THE PAST. VOL. 9. ISSUE 1. P. 223 -241 | 44 | 71% | 8 |
6 | PRESTON, GW , THOMAS, DSG , GOUDIE, AS , ATKINSON, OAC , LENG, MJ , HODSON, MJ , WALKINGTON, H , CHARPENTIER, V , MERY, S , BORGI, F , ET AL (2015) A MULTI-PROXY ANALYSIS OF THE HOLOCENE HUMID PHASE FROM THE UNITED ARAB EMIRATES AND ITS IMPLICATIONS FOR SOUTHEAST ARABIA'S NEOLITHIC POPULATIONS.QUATERNARY INTERNATIONAL. VOL. 382. ISSUE . P. 277 -292 | 45 | 63% | 5 |
7 | BOSTOEN, K , CLIST, B , DOUMENGE, C , GROLLEMUND, R , HOMBERT, JM , MULUWA, JK , MALEY, J , (2015) MIDDLE TO LATE HOLOCENE PALEOCLIMATIC CHANGE AND THE EARLY BANTU EXPANSION IN THE RAIN FORESTS OF WESTERN CENTRAL AFRICA.CURRENT ANTHROPOLOGY. VOL. 56. ISSUE 3. P. 354 -384 | 43 | 67% | 4 |
8 | JOLLY, D , HARRISON, SP , DAMNATI, B , BONNEFILLE, R , (1998) SIMULATED CLIMATE AND BIOMES OF AFRICA DURING THE LATE QUATERNARY: COMPARISON WITH POLLEN AND LAKE STATUS DATA.QUATERNARY SCIENCE REVIEWS. VOL. 17. ISSUE 6-7. P. 629 -657 | 63 | 63% | 163 |
9 | MORRISSEY, A , SCHOLZ, CA , (2014) PALEOHYDROLOGY OF LAKE TURKANA AND ITS INFLUENCE ON THE NILE RIVER SYSTEM.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY. VOL. 403. ISSUE . P. 88 -100 | 36 | 80% | 9 |
10 | NICOLL, K , (2004) RECENT ENVIRONMENTAL CHANGE AND PREHISTORIC HUMAN ACTIVITY IN EGYPT AND NORTHERN SUDAN.QUATERNARY SCIENCE REVIEWS. VOL. 23. ISSUE 5-6. P. 561-580 | 42 | 88% | 59 |
Classes with closest relation at Level 2 |