[ Pûtlā nav ćhûgā

Pīr Satgur Nūr].

[ 12 grañthne 103 ginān

Pīr Ḥasan Kabīr ad-Dīn, Pīr Imām Shāh, Pīr Ṣadr ad-Dīn, ... [et al.]].

[ 12 grañthne 103 (101?) ginān

Pīr Imām Shāh, Pīr Sohodev, Pīr Shams, ... [et al.]].

[ Four ginān books

Pīr Imām Shāh ... [et al.]].

[ Three ginān books

Pīr Imām Shāh ... [et al.]].

[ Mansamjānī vaḍī shamasjī

Pīr Shams].

[ Farmān:jañgbārnā:bījī:mûsāfarinā:tathā:faramān:nāîrobī:mûṁbāsā:pûnā:gûādhar:malīgām(5)nā

Farmāns made by Aga Khan III between February and December 1905 in Zanzibar, Nairobi, Mombasa, Poona and Gwader.

Mûlgāvañtrī:pīr:emām:shāhānī

Publication data missing.

(Table) Radiocarbon datings of sediment core BLK-1 obtained from Barkol Lake, China

The Barkol Lake, as a closed inland lake, is located at the northeast Xinjiang in northwest China. A combination of geochemical indicators including d18O and d13C of carbonate, TOC, carbonate contents, as well as grain size proxies and magnetic susceptibility of sediments obtained from a newly recovered section at this lake, provides a high-resolution history of climatic change in the past 9400 years. Multi-indicators reflect that Holocene climatic change in the study region generally follows the Westerly Wind pattern of Holocene, and three climatic periods can be identified. Between 9400 and 7500 cal a B.P., climate was characterized by relatively drier and colder condition. From 7500 to 5800 cal a B.P., a relatively warmer and moister climate prevailed, but between 5800 and 3500 cal a B.P., climate shifted towards warmer and drier conditions. A relatively colder and wetter climate prevailed during 3500~1000 cal a B.P., then it changed towards cold and dry between 1000 and 500 cal a B.P.; after 500 cal a B.P., climate changed towards warm and dry conditions again. This study reflects that during the Middle Holocene (from ca 7000 to 3500 cal a B.P.), variations of carbonate d18O of sediments from several lakes in the northern Xinjiang were synchronous with that of Qinghai Lake, where was strongly influenced by the South Asian monsoon; however, after 3500 cal a B.P. this consistency was interrupted, possibly resulting from a re-domination of the Westerly Wind and the retreat of South Asian monsoon in the northern Xinjiang.

(Table 2) Age determination of sediment core NIOP-C2_929

In this study we present a sea surface temperature (SST) record from the western Arabian Sea for the last 20,000 years. We produced centennial-scale d18O and Mg/Ca SST time series of core NIOP929 with focus on the glacial-interglacial transition. The western Arabian Sea is influenced by the seasonal NE and SW monsoon wind systems. Lowest SSTs occur during the SW monsoon season because of upwelling of cold water, and highest SSTs can be found in the low-productivity intermonsoon season. The Mg/Ca-based temperature record reflects the integrated SST of the SW and NE monsoon seasons. The results show a glacial-interglacial SST difference of ~2°C, which is corroborated by findings from other Arabian Sea cores. At 19 ka B.P. a yet undescribed warm event of several hundred years duration is found, which is also reflected in the d18O record. A second centennial-scale high SST/low d18O event is observed at 17 ka B.P. This event forms the onset of the stepwise yet persistent trend toward Holocene temperatures. Highest Mg/Ca-derived SSTs in the NIOP929 record occurred between 13 and 10 ka B.P. Interglacial SST is ~24°C, indicating influence of upwelling. The onset of Arabian Sea warming occurs when the North Atlantic is experiencing minimum temperatures. The rapid temperature variations at 19, 17, and 13 ka B.P. are difficult to explain with monsoon changes alone and are most likely also linked to regional hydrographic changes, such as trade wind induced variations in warm water advection.

Songs and stories of the Chʻuan Miao.

Without the music.

Le presqu'ile de Malacca : les Malais et les sauvages /

1. ptie. La presqu'ile de Malacca et les Malais.--2. ptie. La presqu'ile de Malacca et les sauvages.

The social and economic organization of two White Meo communities in nothern Thailand /

"Prepared for Advanced Research Projects Agency."

In het rijk van Siameezen en Maleiers /

Met 32 autotypien.

Singalesisk skriftlæare,

Mode of access: Internet.