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1.
This study reviews the occurrence and potential of bryozoans within lithic artifacts and also sets out a methodology for their use in sourcing and discusses the advantages and disadvantages of this approach. We present case studies from our own research and from the literature on using bryozoans in sourcing archaeological lithic artifacts. Fossil bryozoans of different ages and clades can be effectively used to determine the material source of lithic artifacts from a variety of prehistoric ages. The case studies included in this report span the stratigraphic range of bryozoans from the Ordovician to the Neogene. The bryozoans came from four different orders: trepostome, fenestrate, cyclostome, and cheilostome. The use of these lithic artifacts ranged back to 25 ka. Although the majority of the fossil bryozoans were incidental in the artifacts, the bryozoans were still useful for determining their original source rock. The improved searchable online paleontologic databases allow for more efficient use of fossil bryozoans to constrain the stratigraphic and paleogeographic distribution of source outcrops. Although generally underutilized in sourcing prehistoric lithic artifacts, it is clear that by analyzing bryozoans, an increased understanding of the lithologic nature of these materials could be gained by the archaeological community.  相似文献   

2.
东秦岭南洛河中游地区发现的旧石器和黄土堆积   总被引:4,自引:3,他引:1       下载免费PDF全文
对2006~2007年在东秦岭南洛河中游地区河南省卢氏和洛宁两县发现的8处旷野类型旧石器地点的160余件石制品进行了初步研究,并对产出石制品的黄土堆积剖面进行了地层学分析和光释光测年。初步结果表明,南洛河中游地区的旧石器工业很丰富,石制品的加工技术与上游洛南盆地一致,同样采取硬锤直接打击法;加工石制品的原料来自于河流堆积物中的石英岩和石英砾石等;石制品中有相当数量的小型石片和由小型石片二次加工修理而成的工具,还有直接由砾石加工而成的重型工具,如手镐等;除此之外,大型石片以及以大型石片加工而成的重型工具,如重型刮削器也多有所见。由于工作范围和力度的局限,南洛河中游地区目前尚未发现上游洛南盆地旧石器遗址中广泛存在的手斧、三棱手镐、薄刃斧和大型石刀等Acheulian类型两面加工技术生产的工具。新发现的南洛河中游旧石器地点分布在不同时期形成的河流阶地和黄土地层中。地层分析和光释光年代测试表明,南洛河中游地区的黄土堆积至少从中更新世便已经开始,并一直持续到全新世,至少在黄土剖面中S1,S3和S4的3个层位有石器分布;其黄土-古土壤旋回不仅可以用于石制品产出层位的准确定年,还指示了早期人类石器工业演化和人类生存环境变化的过程。  相似文献   

3.
史前人类向青藏高原扩散的过程和适应高海拔缺氧环境的机制是多学科关注的热点科学问题.青海湖盆地是青藏高原旧石器-中石器时代遗址分布最为丰富的区域,对这些遗址出土的石制品原料的分析有助于深入理解青藏高原史前狩猎采集人群的石料开发策略、人群迁徙和交流联系.青海湖盆地151遗址出土的928件石制品的石料研究分析显示,处于末次冰消期的下文化层的石制品以近源的石英和石英岩为主要原料,而处于全新世早中期的上文化层在同类型近源石料仍占主体地位的情况下,开始出现较高比例和多样化的优质硅质石料,并且主要用于生产细石器.野外调查和查阅地质资料均未发现青海湖盆地内有151遗址中出现的同类型优质硅质石料产出,推测其来自远距离搬运.青海湖盆地内其他8个末次冰消期至全新世中期遗址的3269件石制品石料分析结果显示,与151遗址同类型的远源优质硅质石料在全新世早期开始在盆地内的遗址中出现.这一结果表明青海湖盆地末次冰消期古人类活动强度和范围有限,全新世早中期古人类受到全新世大暖期气候变好和周边地区农业人群兴起挤压活动空间的双重影响,在高原上的活动范围和强度大大增加,伴随着开始有意识地开发优质石料,较频繁地进行远距离迁移和人群交流.远源优质硅质石料的产地可能位于北祁连山区和青藏高原上的陆相火山岩区,需要未来更深入的研究揭示.该研究为深入理解青藏高原古人类的高海拔环境适应策略和移动模式提供了重要材料,为理解史前人类向高原扩散的机制提供了重要信息.  相似文献   

4.
Underwater geoarchaeological research in Apalachee Bay, in the northeastern Gulf of Mexico off northwest Florida, has enabled the reconstruction of portions of the karst-controlled paleodrainage system, the discovery of several inundated prehistoric archaeological sites, and the exposure of sediments accumulated during the drowning of the continental shelf. Diagnostic artifacts discovered at the sites included chipped stone tools and debitage indicating Paleoindian, Early Archaic, and Middle Archaic occupation. A geoarchaeological model using terrestrial analogs was used to locate and investigate inundated sites. Methods employed include seismic profiling, vibracoring, diver tow surveys, diver collection transects, and induction dredge excavations. We document evidence for sea-level rise, related environmental succession and site formation processes for indundated prehistoric sites in the Apalachee Bay region from approximately 8000 to 6000 yr B.P. © 1997 John Wiley & Sons, Inc.  相似文献   

5.
Identifying the geological and geographical origin of lithic raw materials is critical to effectively address prehistoric forager raw material economies and mobility strategies. Currently, Paleolithic archaeology in Belgium lacks a systematic sourcing strategy to effectively substantiate detailed interpretations of prehistoric hunter‐gatherer behavioral change across time and space. This pilot study evaluates the potential to “fingerprint” flint from the Mons Basin, western Belgium, using the laser ablation‐inductively coupled plasma‐mass spectrometry (LA‐ICP‐MS) technique and a multivariate statistical analysis of 87 geological samples and 39 Gravettian period chipped stone artifacts. We reappraise two hypotheses raised by previous scholars based on visual raw material identification: (1) the Gravettian occupants of Maisières‐Canal supplied themselves with “black flint” from one single source; (2) the sites Rhens and Koblenz‐Metternich yielded artifacts indicative of long‐distance transfer of western Belgian flint into the German Rhineland, ca. 260 km from the primary source area. Our results demonstrate the validity of LA‐ICP‐MS data with flint and compositional data analysis for fingerprinting discrete geological formations from the Mons Basin. We suggest multiple source provisioning for Maisières‐Canal. Geochemical characterization of other potential flint sources is required to validate the long‐distance transfer hypothesis of western Belgian “black flint” into the German Rhineland.  相似文献   

6.
依据普通薄片、铸体薄片、扫描电镜、X—衍射等分析,对柴西南地区古近—新近系砂岩储层的岩石学特征、成岩作用进行了研究,结果表明:该区储集砂体成分主要由长石岩屑砂岩、岩屑长石砂岩和岩屑砂岩组成,主要成岩作用类型有压实作用、胶结作用、溶蚀作用和交代作用,成岩演化阶段已达到中成岩B期;机械压实作用及胶结作用是早成岩阶段原生孔隙遭受破坏的主要成岩作用类型,溶蚀作用是中成岩阶段形成次生孔隙的主要成岩作用类型;受成岩作用及成岩演化阶段的控制,深部储层出现孔隙度、渗透率高异常发育带。  相似文献   

7.
Archaeological excavations at the Cooper's Ferry site (10IH73), located in the lower Salmon River canyon of western Idaho, revealed a stratified sequence of cultural occupations that included a pit feature containing stemmed points. However, radiocarbon ages determined on charcoal and bone in the pit feature range between ca. 12,000 yr B.P. and 7300 yr B.P. By considering the effects of postdepositional processes on dated samples, and by comparing the lithostratigraphy, pedostratigraphy, and stable isotope geochemistry of pedogenic carbonates from Cooper's Ferry with other well‐dated stratigraphic sections in the canyon, site geochronology is clarified. Based on the presence of key radiocarbon ages and distinctive stratigraphic criteria, we argue that the initial occupation and interment of lithic artifacts in a pit feature at Cooper's Ferry occurred during the late Pleistocene, between ca. 11,410 and 11,370 yr B.P., and not during the early Holocene. Records of geomorphic change and paleoenvironmental proxy data from the site reveal that early occupation in the lower Salmon River canyon corresponds with evolving riparian ecosystems, which must be considered as a contextual aspect of local prehistoric cultural ecology. © 2004 Wiley Periodicals, Inc.  相似文献   

8.
Archaeological surface surveys have located open‐air sites on cropland in the Sierra de Atapuerca (Burgos, Spain). To what degree agricultural disturbances have impacted archaeological site integrity is poorly defined and may greatly affect interpretations of prehistoric land use. This paper presents the results of three experiments concerned with the effects of tillage on artifact distribution, focusing specifically on lateral and vertical artifact displacement. We demonstrate highly variable horizontal displacement of artifacts by plowing and overall downward movement of lithic materials within the soil. This results in an expansion of site boundaries and reduction of surface artifact density, yielding a biased and unrepresentative picture of past human activity. More experimental studies are needed to better define agricultural disturbances to surface archaeological assemblages. © 2008 Wiley Periodicals, Inc.  相似文献   

9.
近20年来中国旧石器考古学的进展与思考   总被引:13,自引:4,他引:13  
本文记述近20年来中国旧石器考古学研究的主要成果,着重论述早期人类扩散的速度和中国旧石器工业的基本框架:北、南方各存在一个主工业,并存若干区域工业;同时对试验考古研究以及东西文化比较研究等的现状和问题提出孔见。  相似文献   

10.
11.
近年来,在东秦岭南洛河流域发现了大批旧石器地点,该区域被认为是中国南北方旧石器工业的交汇和过渡地带。但是,早期人类在这一带的活动时间和环境背景尚不清楚。由于第四纪黄土的定年方法相对成熟,旧石器遗址的黄土堆积可为解决这些问题提供重要证据。对洛南盆地上白川和刘湾两个遗址的黄土剖面进行土壤地层和磁性地层研究以及光释光年龄和磁化率测定结果显示,该地区的黄土堆积可能从110万年前就已经开始,地层有明显的黄土-古土壤旋回,指示了气候和环境在冰期-间冰期时间尺度的变化。黄土地层下部出土的石制品表明,至少在约80万年前后人类就在这一带活动并制作工具。石制品两面加工技术被广泛采用,大量制作精美的手斧和薄刃斧等Acheulian工业类型工具的发现,显示洛南盆地的旧石器工业可能已经突破了"莫氏线(Movius Line)"的框架。  相似文献   

12.
An important question in Southwestern archaeological research is how social and economic ties between prehistoric groups changed through time. The chemical and mineralogical matching of stone tools and ceramics to source areas is one approach to addressing this question. Here we challenge the assumption that igneous rocks used for manufacturing stone tools and ceramics in the Mesa Verde region of Colorado were originally derived from the Chuska Mountains of New Mexico. Recent geological surveys suggest that small igneous features present in and around Mesa Verde National Park and Ute Mountain Ute Tribal Park contain similar lithologies and may represent a local source. We systematically visited seven of these igneous exposures and nine downstream gravel deposits, looking for geological sources and quarry sites matching the lithology of analyzed debitage from this region. Our results suggest that the ancestral Puebloans could have procured such igneous rocks as aphanitic minette and trachybasalt pottery temper from local areas. Because the trachybasalt is usually thought to have been imported from the Chuska Mountains, this discovery may require a revision of interpreted trade networks based on pottery temper and lithic raw material distinctions. © 2009 Wiley Periodicals, Inc.  相似文献   

13.
Hunter‐gatherer mobility and spheres of interaction are important characteristics worthy of investigation in Patagonian archaeology. One way to approach these is by studying the distribution of lithic archaeological materials. Siltstone (limolite) artifacts are found along the western strip of southwestern Patagonia, Argentina. Based on geomorphological studies and the high density of archaeological material, a source was located along the western margin of Cardiel Lake. Neutron activation analysis of samples from the source and archaeological sites in several neighboring basins allowed us to model its circulation. Siltstone's archaeological distribution indicates that its regional circulation had a southerly direction dating from the early Holocene. This southern vector shows an important difference when compared to the distribution of obsidian from Pampa del Asador, which has a broader circulation pattern. This could be related to a greater availability of high‐quality lithic materials north of the siltstone source. This work also contributes to the construction of a lithic source database for southern Patagonia.  相似文献   

14.
南海北部渐新世/中新世之交发生了物源突变地质事件。利用珠江口盆地白云凹陷渐新统珠海组和中新统珠江组砂岩薄片镜下计点法统计技术,详细研究了碎屑组分的变化特征。结果表明:珠海组砂岩碎屑组分中,岩屑以深成的岩浆岩屑占绝对优势,长石和沉积岩屑含量也相对较高,与该期物源主要来自华南沿海近源以燕山期花岗岩为主的母岩区相一致;而珠江组砂岩中,岩屑以变质岩屑占优势,同时也含有一定量的岩浆岩屑、沉积岩屑和较多的长石,显示珠江组具有更多的物源供给区。随着渐新世/中新世之交各种地质事件发生,尤其是伴随青藏高原隆升引起的大陆风化及侵蚀程度增强,珠江口盆地沉积物源区向华南古陆内部古老的沉积-变质岩区和青藏高原东麓扩展,碎屑组分变化应该是该期各种地质事件的综合作用结果。  相似文献   

15.
Pottery from the Bronze Age of southwest Spain has traditionally been approached from a “typological” stand seeking the establishment of chronological sequences. This article examines ceramics from two different Bronze Age sites, a settlement (El Trastejón) and a necropolis (La Traviesa), from an archaeometric viewpoint. The methodology involved includes mineralogical characterization by XRD and optical microscopy, chemical analysis by XRF, and morphometric analysis through digital processing of thin sections. The analytical results are contextualized within the general framework of our current archaeological knowledge of both sites and their general background, and then a preliminary interpretation is proposed in terms of the prehistoric technology of pottery manufacture and functionality. © 2005 Wiley Periodicals, Inc.  相似文献   

16.
基于岩石薄片观察、压汞分析、扫描电镜和X衍射分析等方法对罗子沟盆地大砬子组砂岩物性特征进行了定性-定量研究。结果表明:罗子沟盆地大砬子组砂岩成分成熟度和结构成熟度低,以岩屑长石砂岩和长石砂岩为主;岩石孔隙度高,孔隙度主要为16.2%~26.4%,次生孔隙占总孔隙度面孔率的88%,但总体渗透率极低,渗透率主要分布在(0.13~1.68)×10-3 μm2,为高孔特低渗的物性特征。有机元素分析、色谱分析、岩石热解及显微组分镜检分析表明,罗子沟盆地大砬子组泥页岩中有机质在热演化过程中产生大量有机酸,有机酸对砂岩中长石等矿物的溶蚀作用是次生孔隙发育的主要原因,但有机酸溶蚀产生的次生矿物在一定程度上堵塞了孔隙喉道。因此,研究区砂岩形成高孔特低渗的物性特征。  相似文献   

17.
Classification and sourcing of vulcanic lithics is simplified through petrographic and geochemical analyses. In examining volcanic lithics, major element geochemistry is required for classification, trace element geochemistry is necessary for discrimination of materials from different sources, and rare earth elements are used in source-modeling. Materials such as those found in the debitage at the British Camp shell midden, San Juan Island (45SJ24), are ubiquitous in the Gulf of Georgia region of the Pacific Northwest. Previous archaeological reports over the past 100 years have classified this volcanic debitage as basalt and predicted a local source. Petrographic analyses of thin sections and geochemical analyses using ICP emission spectrometry have shown that these artifacts are formed of dacite rather than basalt. The analysis also shows that the major lithic material used for stone chipping during the entire temporal sequence at the British Camp site is invariably from the same distant source in the High Cascades, possibly as far as 200 km from the site. © 1996 John Wiley & Sons, Inc.  相似文献   

18.
Characterizing raw material of stone tools used by Late Neolithic and Copper Age communities is important for interpreting access to available sources and establishing regional routes of distribution. Ichnological analysis may be used to help characterize lithic material and determine the source of artifacts. Here we report for the first time the existence of trace fossils in artifacts from the Late Neolithic and Copper Age of southern Spain. Ichnological analysis indicates a trace fossil assemblage consisting of relatively scarce small‐sized Chondrites and abundant Phycosiphon. A regional survey of natural outcrops and chert quarries indicates the presence of discrete trace fossils only in the samples from geological formations that are part of the Campo de Gibraltar Complex. Ichnological composition in these samples is similar to that discerned in the artifacts and suggests that this was the probable source of the chert used in tool manufacture. © 2010 Wiley Periodicals, Inc.  相似文献   

19.
Archaeological sites composed only of surficial lithics are widespread in arid environments. Numerical dating of such sites is challenging, however, and even establishing a relative chronology can be daunting. One potentially helpful method for assigning relative chronologies is to use lithic weathering, on the assumption that the most weathered artifacts are also the oldest. Yet, few studies have systematically assessed how local environmental processes affect weathering of surficial lithics. Using macroscopic analyses, we compared the weathering of surficial lithic assemblages from seven mid‐to‐late Holocene archaeological sites sampled from four different microenvironments in the Atacama Desert of northern Chile. Changes in polish, texture, shine, and color were used to establish significant differences in weathering between two kinds of locations: interfluves and canyon sites. Lithics from interfluve sites were moderately to highly weathered by wind and possessed a dark coating, whereas canyon lithics were mildly weathered despite greater exposure to moisture, often lacked indications of eolian abrasion, and lacked dark coatings. Our results show that lithic weathering can be used as a proxy for relative age, but only after considering local environmental factors. The power of such chronologies can be improved by combining archaeological, paleoenvironmental, geomorphological, and taphonomic data.  相似文献   

20.
An extensive ancient archeologic site containing lithic artifacts and associated with mammoth remains was reported at Chinitna Bay, southern Alaska in 1943. The presence of such a site adjacent to the continental shelf at the base of the rugged Aleutian Range suggested that humans may have inhabited the inner shelf environment during the late Pleistocene at times of lowered sea level. Because of the site's potential significance, an interdisciplinary research team relocated and reinvestigated the area in 1978, but failed to find evidence of prehistoric human habitation. Geologic studies and radiocarbon dating indicate that the strata reported at the site are intertidal in origin, very late Holocene in age, and have undergone significant tectonic movement in the recent past. These observations indicate that the previously published observations of the Chinitna Bay site are probably invalid.  相似文献   

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