High tropical and low polar biodiversity is one of the most fundamental patterns characterizing marine ecosystems, and the influence of temperature on such marine latitudinal diversity gradients is increasingly well documented. However, the temporal stability of quantitative relationships among diversity, latitude and temperature is largely unknown. Here we document marine zooplankton species diversity patterns at four time slices [modern, Last Glacial Maximum (18,000 years ago), last interglacial (120,000 years ago), and Pliocene (~3.3-3.0 million years ago)] and show that, although the diversity-latitude relationship has been dynamic, diversity-temperature relationships are remarkably constant over the past three million years. These resu...
Aim: Poleward migration is a clear response of marine organisms to current global warming but the ge...
Proposed explanations for the geographic distribution of zooplankton diversity include control of di...
Marine environments have increased in temperature by an average of 1°C since pre-industrial (1850) t...
High tropical and low polar biodiversity is one of the most fundamental patterns characterizing mari...
Extensive investigation of the close association between biological diversity and environmental temp...
Planktic foraminiferal species diversity dataset of the Pliocene time slice. Lat: latitude. Long: lo...
Planktic foraminiferal species diversity dataset of the Last Glacial Maximum time slice. Lat: latitu...
The Cenozoic planktonic foraminifera (PF) (calcareous zooplankton) have arguably the most detailed f...
A benthic microfaunal record from the equatorial Atlantic Ocean over the past four glacial-interglac...
There is a growing evidence that changes in deep-sea benthic ecosystems are modulated by climate cha...
Planktic foraminiferal species diversity dataset of the last interglacial time slice. Lat: latitude....
Biodiversity is expected to change in response to future global warming. However, it is difficult to...
The geographic distribution of life on Earth supports a general pattern of increase in biodiversity ...
Harmonized data and R code for "Plankton response to global warming is characterized by non-uniform ...
Biodiversity has been changing both in space and time. For example, we have more species in the trop...
Aim: Poleward migration is a clear response of marine organisms to current global warming but the ge...
Proposed explanations for the geographic distribution of zooplankton diversity include control of di...
Marine environments have increased in temperature by an average of 1°C since pre-industrial (1850) t...
High tropical and low polar biodiversity is one of the most fundamental patterns characterizing mari...
Extensive investigation of the close association between biological diversity and environmental temp...
Planktic foraminiferal species diversity dataset of the Pliocene time slice. Lat: latitude. Long: lo...
Planktic foraminiferal species diversity dataset of the Last Glacial Maximum time slice. Lat: latitu...
The Cenozoic planktonic foraminifera (PF) (calcareous zooplankton) have arguably the most detailed f...
A benthic microfaunal record from the equatorial Atlantic Ocean over the past four glacial-interglac...
There is a growing evidence that changes in deep-sea benthic ecosystems are modulated by climate cha...
Planktic foraminiferal species diversity dataset of the last interglacial time slice. Lat: latitude....
Biodiversity is expected to change in response to future global warming. However, it is difficult to...
The geographic distribution of life on Earth supports a general pattern of increase in biodiversity ...
Harmonized data and R code for "Plankton response to global warming is characterized by non-uniform ...
Biodiversity has been changing both in space and time. For example, we have more species in the trop...
Aim: Poleward migration is a clear response of marine organisms to current global warming but the ge...
Proposed explanations for the geographic distribution of zooplankton diversity include control of di...
Marine environments have increased in temperature by an average of 1°C since pre-industrial (1850) t...