Characteristics of Fossil Wood from Loa Sugarcane Kutai Kertanegara, East Kalimantan

Nani Husien, Muhammad Nur Hidayat, Agus Sulistyo Budi, Erwin
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Abstract

Fossil Wood is wood that has petrified as a result of wood or plant stems being buried by sediment, does not experience decay and the cells in the wood are replaced by minerals over a long period of time but the outer structure of the wood is still maintained. One way to find out the characteristics of fossil wood is by observing or characterizing it both macroscopically and microscopically. This study aims to determine the macroscopic characteristics, hardness values and density of wood fossils found in Loa Tebu Village, Kutai Ketanegara. Observations of macroscopic characteristics included the color of wood fossils which were observed by naked eye and with a loupe magnification of 10x, and observations of other macroscopic characteristics were carried out on three areas of wood namely transverse, tangential and radial planes using a Nikon SMZ 645 Stereo Microscope with a magnification of 30x. The hardness value uses a rock hardness test tool, namely "Diamond Selector II", while the density uses the general calculation standard for specific gravity, namely the ratio of mass to volume. The results showed that the characteristics of the fossil wood from Loa Tebu were light brown, dark brown, white and gray in color. The color found in the wood fossils is probably caused by cells that have been mixed with inorganic elements and mineral constituents around the location of the wood fossils. Another macroscopic structural observation was the discovery of wood cells such as those of broad leaf wood in general, namely the presence of vessel cells (pores), radius cells and clusters of fiber cells. Axial intercellular channels (SIA) were also found in the samples and arranged tangentially. The AIA characteristics found here are common characteristics that are often found in several species of wood from the Dipterocarpaceae family. The results of the measurement of the sample hardness value were 4 on the Mohs scale and the density was 3.26
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东加里曼丹Kutai Kertanegara地区Loa甘蔗化石木材特征
化石木是由于木材或植物茎被沉积物掩埋而石化的木材,没有经历腐烂,木材中的细胞在很长一段时间内被矿物质取代,但木材的外部结构仍然保持不变。找出木材化石特征的一种方法是从宏观和微观两方面对其进行观察或表征。本研究旨在确定在Kutai Ketanegara Loa Tebu村发现的木材化石的宏观特征、硬度值和密度。宏观特征的观察包括用肉眼观察木材化石的颜色,用放大镜放大10倍,其他宏观特征的观察使用尼康SMZ 645立体显微镜放大30倍,在木材的横向、切向和径向三个区域进行。硬度值采用岩石硬度测试工具,即“金刚石选择器II”,而密度采用比重的一般计算标准,即质量与体积之比。结果表明,罗阿特布古木材的主要特征为浅棕色、深棕色、白色和灰色。在木化石中发现的颜色可能是由细胞与木化石周围的无机元素和矿物成分混合而成的。另一个宏观结构观察是木材细胞的发现,如一般阔叶木材的细胞,即血管细胞(孔隙)、半径细胞和纤维细胞簇的存在。在样品中还发现了轴向细胞间通道(SIA),它们呈切向排列。这里发现的AIA特征是在双龙心科的几种木材中经常发现的共同特征。测定样品的莫氏硬度值为4,密度为3.26
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