一个小南极岛 (半月) 的小生物多样性和鸟类生成:地形-地质-植被的相互关系

Daniela Schmitz1,2,3, Rafael G Siqueira1,4, Roberto F M Michel5

  • 1Universidade Federal de Viçosa (UFV), Núcleo Terrantar, Departamento de Solos, Vila Gianetti, 8, 36570-075 Viçosa, MG, Brazil.

概括

企瓜诺显著塑造了半月岛上的南极土壤,创造了各种各样的土壤类型,如Cryosols和Leptosols. 这凸显了海鸟群体在极地地区营养循环和陆地生态系统发展中的关键作用.

相关概念视频

Conservation of Declining Populations02:07

Conservation of Declining Populations

Conservation of declining population focuses on ways of detecting, diagnosing, and halting a population decline. The approach uses methods to prevent populations from going extinct.
9.6K
The Evidence for Evolution02:55

The Evidence for Evolution

Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.
42.5K
What is Evolutionary History?02:35

What is Evolutionary History?

Scientists record evolutionary history by analyzing fossil, morphological, and genetic data. The fossil record documents the history of life on Earth and provides evidence for evolution. However, both fossil and living organisms offer evidence that outlines Earth’s evolutionary history.
36.2K
Speciation Rates01:07

Speciation Rates

Overview
21.0K
Formation of Species01:31

Formation of Species

Speciation describes the formation of one or more new species from one or sometimes multiple original species. The resulting species are discrete from the parent species, and barriers to reproduction will typically exist. There are two primary mechanisms, speciation with and without geographic isolation—allopatric and sympatric speciation, respectively.
39.0K
The Colonization of Land02:22

The Colonization of Land

Changes in the environment of the early Earth drove the evolution of organisms. As prokaryotic organisms in the oceans began to photosynthesize, they produced oxygen. Eventually, oxygen saturated the oceans and entered the air, resulting in an increase in atmospheric oxygen concentration, known as the oxygen revolution approximately 2.3 billion years ago. Therefore, organisms that could use oxygen for cellular respiration had an advantage. More than 1.5 years ago, eukaryotic cells and...
34.2K