Louis Calder Center

This article will address the topic of Louis Calder Center, which has become increasingly relevant in today's society. From different perspectives and contexts, Louis Calder Center has become a point of interest for leaders, researchers, academics and the general public. Throughout history, Louis Calder Center has been the subject of discussion and debate, fueling conversations and questions that have led to significant advances in various areas. In this sense, it is essential to delve deeper into the analysis of Louis Calder Center, considering its current impact and the possible future implications that it allows us to glimpse. Thus, this article will seek to offer a comprehensive and updated vision of Louis Calder Center, with the purpose of promoting greater understanding and reflection on this topic that is so relevant in contemporary society.

The Louis Calder Center is Fordham University's biological field station. The Calder Center is a protected forest preserve located 30 miles (48 km) north of New York City in Armonk, New York, and is the only full-time ecological research field station in the New York metropolitan area.

History

The Louis Calder Center was founded in 1967 when paper magnate Louis Calder donated his 113-acre (0.46 km2) estate to Fordham University. Buildings have since been constructed, renovated, and modernized.

Buildings

The Louis Calder Center consists of 19 buildings including:

Calder Lake

Calder Lake is a 4 hectare mesoeutrophic lake located within the Louis Calder Center. The lake bottom is more than half covered by a submersed macrophyte community, including Vallisneria americana, Elodea canadensis, Potamogeton amplifolius, and Najas flexilis. Since Calder Lake is relatively small, the surrounding flora (including Quercus rubra, Quercus prinus, Acer rubrum, Fagus grandifolia, and Cornus florida) plays a significant role in its ecology, as falling leaves add nutrients to the water. The production rates of bacteria and larger phytoplankton in the lake are limited by the supply of inorganic phosphorus. Dissolved organic carbon exists between 4–6 mg C/L in the lake.

External links

41°07′28″N 73°43′49″W / 41.124571°N 73.730297°W / 41.124571; -73.730297