At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所的生物体主要包括：化学转化、向光性和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世生物礁造礁生物研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微生物间共生的典型例子，它是真和蓝或藻类的共生体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的体主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世礁造礁究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微间共的典型例子，它是真菌和蓝细菌或藻类的共体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的体主要：学转细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世礁造礁研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微间共的典型例子，它是真菌和蓝细菌或藻类的共体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了的微小 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的生物体主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世生物礁造礁生物研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微生物间共生的典型子，它是真菌和蓝细菌或藻类的共生体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的生物体主要包括：化学转化细菌、向光性细菌和。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世生物礁造礁生物研究主要以主，如叶状、管孔等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微生物间共生的典型例子，它是真菌和蓝细菌或的共生体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的体主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世造研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微间共的典型例子，它是真菌和蓝细菌或藻类的共体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

球历史上的个时候，上帝海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的生物体主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世生物礁礁生物研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

衣就是微生物间共生的典型例子，它是真菌和蓝细菌或藻类的共生体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的生物体主要包括：化学转化细、向光性细类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世生物礁造礁生物研究主要以类为主，如叶状、管孔等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微生物间共生的典型例子，它是真蓝细或类的共生体。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了海洋中的微小海 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利的主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世礁造礁研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是微间共的典型例子，它是菌和蓝细菌或藻类的共。

At some unspecified time in earth s past, God created microscopic algas in the oceans.

在地球历史上的个时候，上帝创造了洋中的 藻 。

The microorgan-isms employed include mainly chemical conversion bacteria,phototropic bacteria and alga.

所利用的体主要包括：化学转化细菌、向光性细菌和藻类。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚石炭世礁造礁研究主要以藻类为主，如叶状藻、管孔藻等。

The lichen is a typical example of the intergrowth among the microorganism, it is fungi, blue bacterium or homobium of the alga.

地衣就是间共的典型例子，它是真菌和蓝细菌或藻类的共体。