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Hendri Asyhari Fajrian Kaharudin
"
ABSTRACT
his study explores prehistoric human subsistence adaptations within the context of changing marine and terrestrial environments on the tiny Island of Kisar, beginning during the Pleistocene-Holocene transition around 15,000 years ago (ka). We use zooarchaeological data on faunal remains (vertebrates and invertebrates) recovered from Here Sorot Entapa rockshelter (HSE) in temporal relationship to climate data from Flores to document prehistoric human responses to regional sea-level, temperature, and associated habitat changes that occurred after the Last Glacial Maximum (LGM). Human settlement intensity peaked during the colder drier conditions of the Bolling-Allerod period at 14.4-13 ka, and the site was abandoned during a period of unstable sea levels and coastal habitats between 9.4-5 ka. Holocene climate change coincides with increased reefal subsistence, and an increase in crab exploitation over sea urchin use. Rodent abundance increases in the early Holocene, possibly in response to expanding forests during warmer wetter conditions, with a significant increase in the late Holocene as a result of the human introduction of exotic species to the island."
Depok: University of Indonesia, Faculty of Humanities, 2019
909 UI-WACANA 20:3 (2019)
Artikel Jurnal  Universitas Indonesia Library
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Qinanti Anakke Duan Yarita Tawekal
"Perairan utara Papua berada pada lokasi yang strategis, dimana merupakan posisi salah satu pintu masuk arus lintas Indonesia (arlindo) yang merupakan bagian dari siklus oseanografi global. Sedimen laut dapat memberikan data mengenai keadaan lingkungan sekitarnya yang relatif lengkap dan tidak terganggu hingga jutaan tahun. Bukti perubahan lingkungan yang terekam pada sedimen laut berdasarkan karakteristik sedimen dan kandungan foraminifera pada periode transisi Pleistosen dan Holosen juga masih belum banyak dipelajari. Periode transisi Pleistosen-Holosen dapat menimbulkan dampak perubahan lingkungan yang dapat diteliti perbedaan akibat perubahan iklim tersebut. Kondisi tersebut dapat menimbulkan dampak perubahan lingkungan, paleogeografi, dan sumber daya alam yang signifikan. Variasi kelimpahan dan kumpulan foraminifera sendiri merupakan respons adaptif dari foraminifera terhadap perubahan lingkungan dengan habitatnya. Sedimen yang terdapat pada perairan Utara hingga Barat Jayapura ini kemudian dianalisis menggunakan metode Analisis Foraminifera, XRF, Granulometri dan LOI. Berdasarkan hasil kurva dari keempat metode yang dilakukan, dicurigai batas antara Kala Pleistosen dan Holosen berada di kedalaman 61 cm. Hasil tersebut yang digunakan untuk mengidentifikasi perbedaan komposisi foraminifera dan karakteristik sedimen akibat perubahan iklim yang terjadi.

The waters of northern Papua are in a strategic location, which is the position of one of the entrances to the Indonesian cross flow (arlindo) which is part of the global oceanographic cycle. Marine sediments can provide data about the condition of the surrounding environment that is relatively complete and undisturbed for millions of years. Evidence of environmental changes recorded in marine sediments based on sediment characteristics and foraminifera content during the Pleistocene and Holocene transition periods has also not been widely studied. The Pleistocene - Holocene transition period can cause the impact of environmental changes which can be studied for differences due to climate change. These conditions can result in significant changes in the environment, paleogeography and natural resources. Variations in the abundance and collection of foraminifera themselves are an adaptive response of foraminifera to environmental changes in their habitat. The sediment found in the waters north to west of Jayapura was then analyzed using Foraminifera Analysis, XRF, Granulometry and LOI methods. Based on the curve results from the four methods used, it is suspected that the boundary between the Pleistocene and Holocene times is at a depth of 61 cm. These results are used to identify differences in foraminifera composition and sediment characteristics due to climate change."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2024
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UI - Skripsi Membership  Universitas Indonesia Library
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"The Conference of Parties (COP) 15 of the United Nations Framework Convention on Climate Change (UNFCCC), held in Copenhagen in December 2009, ended with no legally-binding commitments. The confer­ence has produced the Copenhagen Accord, but left many issues unad­dressed, and thus, creating uncertainty concerning the future of the Kyoto Protocol. This is certainly not a very promising outcome, since the COP 13 in Bali has mandated a legally-binding agreement to be concluded in COP 15.
The results of the conference have sparked critiques, while the world leaders started to blame each other for the collapse of the climate talks in Copenhagen. Developing countries pointed at the developed countries for the uneasy results of the Copenhagen meeting, as clearly indicated by the statement of the spokesperson of the G77 who blamed the US President for `locking the poor into permanent poverty by refusing to reduce US emissions further'. On the other hand, leaders of developed countries blamed the fast-growing developing countries for the failure.' Still, however, other countries see the Accord as the best possible result of otherwise worse alternatives that could be achieved in Copenhagen.2 Hence, they declared their association with the Accord and subsequently submitted their emission reduction plans. Indonesia belongs to this latter group by submitting its unilateral pledge to cut emissions by 26 to 41 per cent of its Business as Usual (BAU) emissions in 2020.
Given all controversies surrounding the Accord, one may ask why a developing country like Indonesia needs to be associated with the Accord in the first place. Further, questions may also arise as to the legal status
of the Accord and the position of developing countries in the next climate talks. In addition, one may also pose a question as to whether Indonesia could achieve its pledge by considering policies and laws related to Greenhouse Gases (GHGs) mitigation in Indonesia.
To answer these questions, this chapter is structured as follows. After this introduction, Section 1 will discuss various important issues in the Copenhagen Accord. The discussions will be followed by an overview of some challenges that probably surface in the next climate talks. Section 2 attempts to provide a proposal on emission reduction targets that are more consistent with the common but differentiated principle, given the needs to keep the increased temperature below 2° Centigrade. Section 3 discusses some policies and laws related to GHGs mitigation in Indonesia. Section 4 analyses Indonesian legal responses to climate change. Some concluding remarks will be provided in Section 5."
Northhampton: [Edward Elgar, Universitas Indonesia],
MK-Pdf
UI - Makalah dan Kertas Kerja  Universitas Indonesia Library
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Tomkiewicz, Micha
New York: Momentum Press, 2011
551.6 TOM c
Buku Teks  Universitas Indonesia Library
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Berlin: Konrad Adenauer Stiftung, 2016
551.6 INT
Buku Teks  Universitas Indonesia Library
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Juhyeon, KANG
Jakarta: Elex Media Komputindo, 2019
551.6 JUH w
Buku Teks  Universitas Indonesia Library
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"Effect of climate change on water balance will play a key role in the biosphere system. To study the global climate change impact on water balance during 95-year period (1901-1995) long-term grid climatic data including global mean monthly temperature and precipitation at 0.5x0.5 degree resolution were analyted
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INJOAGS
Artikel Jurnal  Universitas Indonesia Library
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Butarbutar, Tigor
Jakarta: Jurnal Analisis Kebijakan Kehutanan, 2009
JAKK 6(1-3)2009
Artikel Jurnal  Universitas Indonesia Library
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