Quantitative reconstruction of primary productivity in low latitudes during the last glacial maximum and the mid-to-late Holocene from a global Florisphaera profunda calibration dataset
Autor: | Blanca Ausín, Iván Hernández-Almeida, Heather Stoll, Mariem Saavedra-Pellitero, Karl-Heinz Baumann |
---|---|
Rok vydání: | 2019 |
Předmět: |
010506 paleontology
Archeology Global and Planetary Change 010504 meteorology & atmospheric sciences Primary production Geology Last Glacial Maximum 01 natural sciences Carbon cycle Latitude Paleoceanography Environmental science Physical geography Late Glacial Maximum Relative species abundance Ecology Evolution Behavior and Systematics Holocene 0105 earth and related environmental sciences |
Zdroj: | Quaternary Science Reviews. 205:166-181 |
ISSN: | 0277-3791 |
DOI: | 10.1016/j.quascirev.2018.12.016 |
Popis: | Ocean net primary productivity (Npp) is a key component of the marine carbon cycle. Multi-model Npp projections based on a few decades of satellite data show large uncertainties, in particular at low latitudes (30°N−30°S). Calibration of sedimentary proxies with satellite-based Npp estimates allows for the quantitative reconstruction of this variable at longer time-scales. Relative abundance of deep-photic zone coccolithophore species Florisphaera profunda in the fossil record can potentially be used as a quantitative proxy for Npp. However, the robustness of this proxy calibration has been tested in very specific oceanographic settings using surface sediment samples. Here, we use a global dataset of surface sediment (n = 1258) and sediment trap (n = 26) samples with relative abundance data of F. profunda (%) to test the robustness of this proxy as a quantitative indicator of Npp. We study the modern and paleo-ecology of this species and the main factors affecting its latitudinal distribution. Results show that F. profunda % is a strong indicator of Npp at latitudes between 30°N and 30°S, while at higher latitudes temperature-related variables are more important. We develop a global calibration model between satellite Npp estimates and F. profunda for the latitudinal range between 30°N and 30°S, and we apply it to several low-latitude sediment cores with available F. profunda counts covering the Late Glacial Maximum (LGM; 24–19 ka) and the Mid-to-Late Holocene period (MLH |
Databáze: | OpenAIRE |
Externí odkaz: |