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Nah, pada postingan kali ini admin akan membagikan ebook karya Gorky, yang berjudul Ibunda tersebut. Ia menggambarkan kehidupan orang-orang akar rumput, ketimpangan sosial, menceritakan kesusahan mereka, brutal serta getar kemanusiaan dalam kehidupan mereka. Ia menulis, bukan karena keindahan dan estetika -meskipun ia sangat memperhatikan aspek ini- namun lebih pada tekanan laku politik dan moral yang diandaikan dapat mengubah dunia. Nama penanya merefleksikan kegeramannya terhadap kehidupan di Rusia dan tekadnya untuk menyampaikan kebenaran yang meskipun pahit adanya.īuku pertamanya, Essays and Stories (1898) menggapai sukses, kariernya sebagai penulis dimulai dari sini. Ia mulai menggunakan nama Gorky, yang berarti "pahit" mulai tahun 1892, ia bekerja di koran The Caucasus. Gorky pun menjalani profesi sebagai wartawan dengan nama pena Jehudiel Khlamida. Ia berkelana di wilayah kekaisaran Rusia selama 5 tahun, berganti-ganti pekerjaan, yang nantinya akan membentuk karakter tulisannya. Pada usia 12 tahun, ia melarikan diri dari rumah. Gorki dilahirkan di Nizny Novgorod, ia kehilangan ayah dan ibunya pada usia tujuh tahun. Ia sastrawan yang memperkenalkan aliran Realisme Sosial, sekaligus seorang aktivis politik.
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Gorky bernama asli A lexei Maximovich Peshkov Ia menerjemahkan karya Gorky ke dalam bahasa Indonesia, dengan judul Ibunda.
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Temporal variations probably resulted from changes in upwelling intensity and terrestrial inputs driven by variations in monsoon strength.Gorky diperkenalkan oleh Pramoedya Ananta Toer kepada publik Indonesia. The increase was stronger and the OM less degraded in the East than in the West indicating that continental margin sediments off Java and Flores were the major depocenter of OC burial along the Indian Ocean margin off SW Indonesia. The content of labile OM was low throughout the transect during the LGM and increased during the late Holocene. High biogenic opal covarying with OM content indicates upwelling-induced primary productivity dominated by diatoms to be a major control of OM burial in sediments in the East during the past 20 kyr. The amount and composition of OM was similar along the transect with maximum values during the deglaciation and the late Holocene. They were slightly lower in the East during the Last Glacial Maximum (LGM) and deglaciation, but increased strongly during the Holocene. Sedimentation rates hardly varied over time in the western part of the transect. Sediments were analyzed for bulk composition, stable carbon and nitrogen isotopes of OM, amino acids and hexosamines and terrestrial plant wax n-alkanes and their stable carbon isotope composition. In order to reconstruct the burial and composition of OM during the Late Quaternary, we analyzed five sediment cores from the Indian Ocean continental margin off the Indonesian islands Sumatra to Flores spanning the last 20,000 years (20 kyr). Upwelling regions are sites of high primary productivity and major depocenters of organic carbon (OC), the least understood of which is the Indian Ocean upwelling off Indonesia. Organic matter (OM) storage in sediments displays large regional variations and varied over time during the Quaternary. At present the ocean is forming a major sink in the global carbon cycle. Global climate change is a mosaic of regional changes to a large extent determined by region-specific feedbacks between climate and ecosystems.