白石村遗址与胶东半岛新石器时代早期文化

胶东半岛是一个相对独立的地理单位,目前,对于半岛地区新石器时代的早期文化,存在着不同的认识.通过考察白石文化的文化特征及其与周边文化的联系,可以推定白石文化是胶东半岛新石器文化的源头.     

对旅游客体文化的研究——以胶东半岛为例

旅游文化主要是由旅游主体文化、旅游客体文化与旅游介体文化共同组成的物质财富与精神财富的总和,其中旅游客体文化是旅游文化的基础,也是旅游业赖以生存和发展的依托。近年来随着旅游主体文化需求的多元化和审美情趣的个性化,旅游客体文化建设显示出诸多不足,因此提升旅游客体文化内涵、强化旅游客体文化价值对于促进旅游业健康持续发展,具有重要意义。本文以胶东旅游客体文化建设为例,结合旅游客体文化的特点,从正反两个方面论证旅游客体文化建设的重要性和必要性并给出旅游客体文化建设的合理化建议。     

Evidence of Cat (Felis catus) Fur Exploitation in Medieval Iberia

Whilst the bones of domestic cats (Felis catus ) are recovered from archaeological sites in Iberia routinely, they are rarely subjected to detailed analysis. Consequently, there is limited understanding of the nature of cat–human relations, especially in contrast to northern European regions. In this paper, we present a unique assemblage of 899 cat bones recovered from the medieval site of El Bordellet (Vilafranca del Penedès, Spain) and dated between the end of the 10th century ad and the beginning of the 11th century ad . Zooarchaeological and taphonomic analysis provides the first clear evidence of skinning related to cat fur exploitation in Christian medieval Iberia. Copyright © 2017 John Wiley & Sons, Ltd.     

First Evidence of Collective Human Inhumation from the Cardial Neolithic (Cova Bonica,Barcelona, NE Iberian Peninsula)

Excavations at Cova Bonica (Barcelona, Spain) have revealed 98 human remains, grouped into five age clusters and corresponding to a minimum of six non-articulated individuals. The remains are clearly associated with Cardial pottery, lithic artifacts, and ornaments suggesting an Early Neolithic horizon. The radiocarbon dating of three human individuals provides a reliable attribution to this period, with a range between ca. 5470 and 5220 cal b.c., identifying it as one of the few assemblages of human remains directly dated from this period. These remains correspond to a rare collective human inhumation and join a growing body of samples from the Cardial Neolithic, which is providing some of the important sites for the study of population movement and the spread of Neolithization along the western Mediterranean coast.     

Molluscan death assemblages from uplifted Holocene terraces,Mahia Peninsula,New Zealand,interpreted from present-day intertidal ecology

Beu, A.G., August 2016. Molluscan death assemblages from uplifted Holocene terraces, Mahia Peninsula, New Zealand, interpreted from present-day intertidal ecology. Alcheringa 41, xxx–xxx. ISSN 0311-5518.

Macrofossils from cover beds of marine terraces at Table Cape, Mahia Peninsula, uplifted coseismically ca 250, 1400, 1850 and 3500 years ago are compared with the fauna living on the nearby 200-m-wide intertidal rock platform. The inner platform is dry at low tide, apart from shallow pools containing Diloma aethiops and abundant but unexpected specimens of Zeacumantus subcarinatus and Cominella glandiformis exposed to the sun; all are common fossils in the terrace cover beds. The outer platform is carpeted densely with the alga Hormosira and shelters a diverse fauna, again all common fossils in the terrace cover beds. Sand and gravel containing shell fragments and supporting Zostera sea-grass turf unexpectedly covers ca 5% of the platform in low areas along the east coast. The fossil fauna is listed from 47 samples from two trenches excavated east–west and north–south through the terrace cover beds. Death assemblages of 158 molluscs, including 24 new records as fossils, and 11 taxa in other phyla delimit sediment derived from four shell accumulation sites identified around the present cape: storm beach, high-tidal strand line, hollows in the rock platform and Zostera flats. Up to 32 of the 47 samples (68%) possibly were deposited in Zostera flats; the rest were sand beach accumulations deposited at and near the high-tidal strand line. All fossils common in the cover beds lived on the rock platform. Differences between the deposits in the two trenches result from two factors. Protection along the east coast by protruding tephra beds and an outer rampart armoured with the macroalga Durvillaea prevented erosion of Zostera-supporting sediment which, therefore, was retained after each uplift event. The exposed eastern position of Table Cape also caused sediment to be transported predominantly westwards, onshore on the east coast but away from Table Cape along the north coast.

A.G. Beu [a.beu@gns.cri.nz], Paleontology Department, GNS Science, PO Box 30368, Lower Hutt 5040, New Zealand.     

良渚玉器部分玉料来源的蠡测

良渚文化玉器中,有一种玉器的玉质细腻纯净,透明度较高,颜色为黄绿和深浅不一的绿色。这类玉料的外观与江浙一带所产玉料截然不同,而与辽东半岛岫岩所产软玉极为相似。因此,良渚玉器部分玉料可能采源于辽东半岛。岫岩软玉的传输路线,是从辽东半岛南部沿海出发,渡过渤海海峡到达胶东半岛,再向西南入山东腹地,折向南到江苏北部进入良渚文化分布区。在这条玉材传送路线上起运输中转作用的,是辽东半岛的原始部落和以大汶口、龙山文化为代表的山东地区原始部落。     

雷州半岛区域旅游的竞合态势分析——基于环北部湾经济圈的思考

环北部湾经济圈将成为我国未来经济增长点,但雷州半岛地区目前并未主动融入其中。本文分析了雷州半岛区域旅游在环北部湾经济圈中的竞合态势及竞争优势,并提出其参与环北部湾区域旅游空间竞争与合作的对策。     

History of Deforestation and Reforestation in the Dinaric Karst

The term karst derives from the Kras plateau, which is in the northwestern part of the area now known as the Dinaric Karst. The landscape consists mostly of Mesozoic carbonate rocks and stretches along the Adriatic Sea coast for a distance of 600 km. Although the region lies parallel to the sea, the Mediterranean temperature influence is limited to a narrow coastal belt, except for the amount of precipitation, which can reach 5000 mm yr^?1. Forests belonging to the Mediterranean and Euro‐Siberian – North American region, covered the primary Dinaric Karst. Human deforestation of the Karst began during the Neolithic period, 6500–6000 BC. Throughout history there have been two main reasons for deforestation; economic (the requirements of new land, pastures, timber use and trade), and social (local increases in population, mass migration, wars, raids). Mankind's perception of forest protection and preservation can be traced through documents going back to the 12th century. Reforestation is mentioned in some of them, but successful reforestation did not begin until the 1850s. Nowadays dense natural forests, extensive forest plantations, dry karst shrublands and also completely barren karst areas can all be found on the Dinaric Karst.