Publication Information

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'https://openalex.org/W1870073641', 'https://openalex.org/W1975335631', 'https://openalex.org/W2049826666', 'https://openalex.org/W2085833220', 'https://openalex.org/W2132860428', 'https://openalex.org/W2138990589', 'https://openalex.org/W2509001347', 'https://openalex.org/W2562347756', 'https://openalex.org/W3041840398', 'https://openalex.org/W4251524269'], 'related_works': ['https://openalex.org/W4239649287', 'https://openalex.org/W4238796064', 'https://openalex.org/W4237563445', 'https://openalex.org/W4226016733', 'https://openalex.org/W3215139134', 'https://openalex.org/W3206006857', 'https://openalex.org/W2130076355', 'https://openalex.org/W2082860237', 'https://openalex.org/W2071929903', 'https://openalex.org/W1990804418'], 'abstract_inverted_index': {'伊吹山南麓に位置する滋賀県米原市（旧伊吹町）寺林地域には，寺林I火山灰層および寺林II火山灰層を挟在する中部更新統の寺林層が分布する．寺林I火山灰層と寺林II火山灰層は，高島沖ボーリングコア中のBT60，BT59に対比されており，寺林層の堆積期は酸素同位体比曲線のステージ8の寒冷期から7の温暖期にあたる．本層からは，チョウセンゴヨウPinus': [0], 'koraiensis,': [1], 'コメツガTsuga': [2], 'diversifolia,': [3], 'ウラジロモミAbies': [4], 'homolepisや，ダケカンバBetula': [5], 'ermanii,': [6], 'シラカンバB.': [7], 'platyphylla,': [8], 'ミズメB.': [9], 'grossa,': [10], 'ズミMalus': [11], 'toringo,': [12], 'キイチゴ属Rubusなどの冷温帯～亜寒帯のマツ科常緑針葉樹とカバノキ属・バラ科落葉広葉樹を主体とする大型植物化石とともに花粉化石，昆虫化石が産出する．これらに基づく古環境は，水生植物ホソバミズヒキモPotamogeton': [13], 'octandrusが生育し，それらに依存するノグチアオゴミムシLithochlaenius': [14], 'noguchiiやミズギワゴミムシ属Bembidionが生息する小規模な沼沢と，ハンノキAlnus': [15], 'japonica,': [16], 'キイチゴ属，カヤツリグサ属Cyperus,': [17], 'スゲ属Carex,': [18], 'タデ属Polygonum,': [19], 'ネコノメソウ属Chrysospleniumが生育し，ミズクサハムシ属Plateumarisが共生する湿地が分布していた．また，ヤハズソウKummerovia': [20], 'striata,': [21], 'ヨモギ属Artemisiaなど陽生の草本類が生え，ウラジロモミ，シラカンバ，ミズメの林が広がっていた．主として北側の山地下部では，尾根筋や崩壊斜面にコメツガ，緩傾斜面にウラジロモミ，ハシバミCorylus': [22], 'heterophylla,': [23], 'ズミ，キハダPhellodendron': [24], 'amurense,': [25], '谷筋にはサワグルミPterocarya': [26], 'rhoifolia,': [27], 'オニグルミJuglans': [28], 'mandshurica': [29], 'var.': [30], 'sachalinensisが生育していた．林床には草本類のカラマツソウ属Thalictrum,': [31], 'ツリフネソウImpatiens': [32], 'textoriなどが生え，オサムシ属Carabusが生息する環境が存在した．さらに山地上部ではチョウセンゴヨウ，コメツガ，ダケカンバなどが混生する森林環境が復元できた．また，寺林層最下部層～中部層下部の植物化石群は，冷温帯上部から亜寒帯に相当するやや乾燥した気候を示す．中部層上部では花粉化石においてモミ属，ツガ属，トウヒ属，カバノキ属の減少とブナ属とコナラ亜属の増加がみられ，より湿潤で温暖な気候への変化が示唆される．': [33]}, 'cited_by_api_url': 'https://api.openalex.org/works?filter=cites:W1991945782', 'counts_by_year': [{'year': 2020, 'cited_by_count': 1}], 'updated_date': '2024-12-14T05:54:16.652063', 'created_date': '2016-06-24'}