東亞第三紀(jì)孑遺植物的親緣地理學(xué):現(xiàn)狀與趨勢(shì)
發(fā)布時(shí)間:2018-09-17 19:58
【摘要】:通過分析比較近年來東亞第三紀(jì)孑遺植物的種群遺傳學(xué)與親緣地理學(xué)的研究結(jié)果,總結(jié)了它們的譜系地理格局式樣,分析了其形成的共同地史或氣候成因,并對(duì)未來的研究提出了展望。東亞孑遺植物的譜系地理式樣主要表現(xiàn)為以下4個(gè)方面:(1)中新世中期至晚期的氣候變冷變干驅(qū)使孑遺植物發(fā)生了近期的物種形成,而上新世末以及更新世的氣候變化則促進(jìn)了它們的種內(nèi)譜系分化、遺傳多樣性形成以及種群的收縮與擴(kuò)張,種群的收縮與擴(kuò)張導(dǎo)致部分類群形成地理譜系"縫合帶"。(2)由于不同的植物類群具有不同的生態(tài)位需求以及生物學(xué)特點(diǎn),更新世冰期暴露的東海陸橋?qū)χ袊?日本間斷分布的孑遺植物具有不同的"過濾"與"廊道"效應(yīng),從而導(dǎo)致其呈現(xiàn)不同的遺傳隔離式樣。(3)上新世末青藏高原的快速隆升以及上新世末/更新世初東亞季風(fēng)氣候的加強(qiáng)可能是多個(gè)亞熱帶地區(qū)分布的孑遺植物沿四川盆地附近發(fā)生東西譜系分化的根本原因,也是西北干旱帶分布的孑遺植物發(fā)生東西譜系分化的驅(qū)動(dòng)因素。(4)自晚中新世以來的全球氣候變冷變干驅(qū)使部分第三紀(jì)孑遺植物在更新世以前就已經(jīng)從中國大陸或日本本島遷入臺(tái)灣,并發(fā)生隔離分化,形成了新的物種或地理譜系?傊,歷史與當(dāng)代的地理以及環(huán)境共同影響了東亞第三紀(jì)孑遺植物的地理分布、遺傳多樣性、譜系分化以及物種形成。最后,我們強(qiáng)調(diào)了目前由單位點(diǎn)的簡(jiǎn)單分子鐘模型的運(yùn)用造成的研究不足,并對(duì)未來的研究提出了展望,即基因組數(shù)據(jù)和生物地理模型的使用以及群落水平的整合親緣地理學(xué)研究是未來的研究方向。
[Abstract]:By analyzing and comparing the research results of population genetics and phylogenetic geography of Tertiary relict plants in East Asia in recent years, the patterns of their pedigree geographical pattern are summarized, and the common geological history or climatic causes of their formation are analyzed. The prospect of future research is put forward. The phylogenetic patterns of relict plants in East Asia are as follows: (1) the cold and dry climate from the middle to the late Miocene led to the recent species formation of the relict plants. However, the late Pliocene and Pleistocene climatic changes promoted their intraspecific lineage differentiation, genetic diversity formation, and population contraction and expansion. The contraction and expansion of the population resulted in the formation of "suture zones" in some groups. (2) because different plant groups have different niche needs and biological characteristics, The East China Sea continental bridge exposed during the Pleistocene glacial period has different "filtering" and "corridor" effects on the intermittent distribution of relict plants in China and Japan. This resulted in different genetic segregation patterns. (3) the rapid uplift of the Qinghai-Tibet Plateau at the end of the Pliocene and the enhancement of the East Asian monsoon climate at the end of the Pliocene / early Pleistocene may be the relict plants distributed along Sichuan in several subtropical regions. The root cause of east-west pedigree differentiation in the vicinity of the basin, It is also a driving factor for the east-west lineage differentiation of relict plants in the arid zone of the northwest. (4) the global climate has cooled and dried since the late Miocene, which has driven some Tertiary relict plants from the mainland of China before the Pleistocene. Japan moved to Taiwan, And isolated and differentiated, forming a new species or geographical pedigree. In short, history and contemporary geography and environment affect the geographical distribution, genetic diversity, pedigree differentiation and species formation of Tertiary relict plants in East Asia. Finally, we emphasize the lack of research caused by the use of simple molecular clock models of unit points, and present a prospect for future research. That is, the use of genomic data and biogeographic models as well as the integration of phylogenetic studies at community level are the future research directions.
【作者單位】: 浙江大學(xué)生命科學(xué)學(xué)院瀕危動(dòng)植物保護(hù)生物學(xué)教育部重點(diǎn)實(shí)驗(yàn)室;
【基金】:國家自然科學(xué)基金(31370241,31570214);國家自然科學(xué)基金國際合作項(xiàng)目(31511140095,31561143015)
【分類號(hào)】:Q914
[Abstract]:By analyzing and comparing the research results of population genetics and phylogenetic geography of Tertiary relict plants in East Asia in recent years, the patterns of their pedigree geographical pattern are summarized, and the common geological history or climatic causes of their formation are analyzed. The prospect of future research is put forward. The phylogenetic patterns of relict plants in East Asia are as follows: (1) the cold and dry climate from the middle to the late Miocene led to the recent species formation of the relict plants. However, the late Pliocene and Pleistocene climatic changes promoted their intraspecific lineage differentiation, genetic diversity formation, and population contraction and expansion. The contraction and expansion of the population resulted in the formation of "suture zones" in some groups. (2) because different plant groups have different niche needs and biological characteristics, The East China Sea continental bridge exposed during the Pleistocene glacial period has different "filtering" and "corridor" effects on the intermittent distribution of relict plants in China and Japan. This resulted in different genetic segregation patterns. (3) the rapid uplift of the Qinghai-Tibet Plateau at the end of the Pliocene and the enhancement of the East Asian monsoon climate at the end of the Pliocene / early Pleistocene may be the relict plants distributed along Sichuan in several subtropical regions. The root cause of east-west pedigree differentiation in the vicinity of the basin, It is also a driving factor for the east-west lineage differentiation of relict plants in the arid zone of the northwest. (4) the global climate has cooled and dried since the late Miocene, which has driven some Tertiary relict plants from the mainland of China before the Pleistocene. Japan moved to Taiwan, And isolated and differentiated, forming a new species or geographical pedigree. In short, history and contemporary geography and environment affect the geographical distribution, genetic diversity, pedigree differentiation and species formation of Tertiary relict plants in East Asia. Finally, we emphasize the lack of research caused by the use of simple molecular clock models of unit points, and present a prospect for future research. That is, the use of genomic data and biogeographic models as well as the integration of phylogenetic studies at community level are the future research directions.
【作者單位】: 浙江大學(xué)生命科學(xué)學(xué)院瀕危動(dòng)植物保護(hù)生物學(xué)教育部重點(diǎn)實(shí)驗(yàn)室;
【基金】:國家自然科學(xué)基金(31370241,31570214);國家自然科學(xué)基金國際合作項(xiàng)目(31511140095,31561143015)
【分類號(hào)】:Q914
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